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00:05 | okay, okay, Because I can't couldn't pull up the record button. |
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00:14 | , Well, uh, if everything working on that and I'll just start |
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00:19 | and today we're gonna, uh, out with lectures three, which we |
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00:24 | of go through a number of terms concepts related to the oil industry. |
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00:32 | , and I'm gonna put this on , that's working, but my mouse |
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00:51 | work when I put that on. , So we always like to start |
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00:58 | classes with what is it that we're , uh, teaching and talking about |
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01:05 | what is petroleum? Geology? And is, uh, the definition out |
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01:10 | glucose and Swarbrick. And, basically, it's ah, the geosciences |
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01:20 | we know and learn, and we it Thio finding petroleum and petroleum bearing |
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01:27 | . And, of course, that apply to both conventional unconventional resource is |
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01:37 | here's the value chain again. And gonna reiterate this, uh, on |
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01:42 | test question, I might ask you the four major steps and there's really |
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01:50 | steps, but again on a test to make it simpler. And I |
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01:57 | there's a thing called the rule of . Well, you never try to |
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02:00 | things with more than three parts. this is four parts, so it's |
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02:04 | little complicated. Management sometimes has trouble things that have list more than |
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02:10 | but frontier expiration, expiration, appraisal, development and production. All |
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02:18 | of these air different steps but exploitation are very closely related, and |
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02:25 | are development and production. And in , if you're a developmental geologist, |
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02:30 | probably going to be doing three and . And if you are an exploration |
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02:35 | , you would be doing one and okay, on here is just kind |
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02:44 | looking at the six steps. this is from the highest altitude, |
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02:49 | here we're closing in and getting finer finer grain data. Ah, with |
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02:58 | of these steps Ah, and the front end is where geologists spent |
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03:06 | of their time. And in geophysicists spent ah lot of time in |
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03:13 | and expiration because they were usually the to go out and get figure out |
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03:18 | to do seismic surveys. They were things like gravity and Meg Magnetics to |
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03:25 | to figure out where they were Thio actually do their size make where |
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03:29 | most prospective areas were based on thickness sediment, tree wedges and that sort |
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03:35 | thing. So a lot of work done up here in the front Now |
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03:39 | we, uh now that we have story about kind of nowhere where that |
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03:49 | is so we don't do is much and everything. So we know where |
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03:52 | are. We kind of start at point and we're kind of looking instead |
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03:58 | looking from the outside of the base in as we do here, we're |
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04:02 | the basin and we're looking outwards from we know there's good production to figure |
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04:08 | the extent of it. So we of explore from the center of the |
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04:14 | and work our way out from where have a good sweet spot that we've |
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04:19 | out with looking for better sweet spots that particular unconventional resource. So |
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04:27 | with conventional geological effort is decreasing in direction with the event of 40 seismic |
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04:37 | , lot Mawr eyes going on down in development and production now and with |
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04:45 | . Of course, we've already uh, pretty much where the oil |
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04:52 | gas might be, but we're trying figure out the intricacies of it. |
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04:57 | we spend more time down here with is and we would up here looking |
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05:02 | this. Now, of course, there are a lot of unconventional resource |
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05:07 | out there that we haven't started to yet across the world. And |
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05:14 | there will be people looking from the trying to figure out which one of |
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05:19 | might be worth tapping into and And, uh, as it turns |
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05:24 | , many of the unconventional resource is the United States already had some production |
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05:33 | the way of straight holes without without . So we knew ahead of time |
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05:40 | we're gonna have mm. Some production out of these out of these |
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05:47 | But we knew it wasn't going to enough until we increase that surface area |
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05:51 | using long reach. Well, bores perfect long sections of of a formation |
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06:00 | than just a a short vertical Like, for example, if this |
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06:04 | a layer of rocks right here, of just drilling through here, we |
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06:09 | through there. You automatically increase the sectional surface area between the perforations in |
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06:16 | pipe or the open part of the , however you've completed it and and |
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06:22 | when you frack it, you you three amount of surface area that's |
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06:29 | Thio Ah, lower pressure regime that the fluids to flow. Okay, |
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06:39 | what do we call riel? Geological . Recently, I've seen some geophysical |
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06:46 | , ph. D s and Um, correlate this data with real |
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06:53 | and they're calling real data geophysics. I don't want to offend the Jeff |
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06:57 | this But But because we have geophysics the room and I've worked with a |
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07:03 | of geophysical data in my life you know, we we have Thio |
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07:08 | all this, but you know, you're actually, uh, touching the |
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07:14 | and not bouncing energy off the rocks my mind, that's what really Data |
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07:20 | . And so I hope it doesn't anyone if I call this reald |
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07:25 | But, uh, we've had a graduate student that that tied this unreal |
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07:32 | to geophysical data and, uh so in case there's any confusion there, |
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07:39 | is what I think. Israel data here. Things like a core. |
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07:43 | other words, I pull a piece rock out of the ground I'm actually |
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07:47 | at geology. If I get a wall core, I'm actually looking at |
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07:54 | . If I get cuttings, I actually looking at pieces of rock. |
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07:59 | I go in with wire line I've got a tool that's sitting right |
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08:05 | to the rock, looking at what's next door to the rock. And |
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08:08 | course, now we have things particularly ity, logs ah, that are |
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08:17 | by the array of the fields. , that they have Thio look farther |
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08:23 | into the formation. Uh, but seismic seismic really is. And, |
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08:29 | and in my mind, seismic is form of remote sensing. And it's |
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08:36 | , you know, sometimes you're very away from the actual surface of the |
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08:41 | . For example, if you're doing notion survey, but you are sending |
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08:45 | waves into the into the earth and getting reflections and refraction is back. |
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08:51 | you're, uh, sorting out with fresh refraction and reflection Czar and coming |
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09:00 | with an image that reflects what we when not only when we weigh look |
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09:07 | Coors and sidewalk course. But when look at outcrops and it does it |
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09:10 | a huge scale. Eso. It's neat you can get. Obviously, |
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09:15 | can get seismic lines, whether it's d or two d, you can |
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09:19 | at a section and you're looking at . It's much larger than most outcrops |
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09:26 | could ever imagine seeing and so we and get a really good insight with |
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09:33 | as to, uh, the way these sedimentary deposits and layers and structures |
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09:40 | arranged with each other. And, , the architecture that it forms, |
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09:45 | in sequence strategic fee. Uh, makes it possible for us to understand |
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09:51 | these sentimentally wedges have actually developed before start drilling into them. In other |
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09:57 | , where did the sand come How is it layered? Which way |
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10:01 | it pro grade? Which way did transgress? All sorts of things could |
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10:05 | seen in seismic because it Z like a toolbox that allows you to look |
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10:12 | outcrops on a very large scale scale that you want to. So in |
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10:18 | sense, you are image ing but you're not actually touching it. |
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10:25 | , okay, um and, unfortunately, what happens? Ah, |
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10:31 | of times is when we get into the past when we've done appraisal, |
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10:37 | and production, a lot of times engineers and, uh, another types |
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10:43 | petroleum engineers pretty much handled it. the detail that we look at as |
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10:49 | in the in the in the realm things that we pull out of the |
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10:54 | was very limited. In other geologists. We're always looking at this |
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10:59 | of data to try to understand the of a reservoir. And early |
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11:07 | Ah, lot of reservoir engineers and geologist uh, in production kind of |
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11:17 | of looked at reservoirs as a as it were, and we didn't |
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11:23 | look at or characterize all the heterogeneity that might be in that reservoir |
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11:31 | Okay, so with conventional reservoirs as I pointed out yesterday, a |
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11:39 | of money was put into the front because that's that's usually, um, |
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11:45 | example, if we were Thio, drilling offshore the Atlantic coast. What's |
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11:52 | very first thing we would start spending on? We would start doing |
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11:57 | lot of seismic three D seismic There is a significant amount of two |
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12:04 | already done on the East Coast, then there were even programs and the |
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12:11 | that have pulled together a lot of two d to simulate the three |
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12:17 | uh, image ing of the two data. But what with that two |
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12:23 | data LAX is, uh, the added quality of riel three D |
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12:32 | especially when it's ah, mhm multi movil and looks from every different |
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12:40 | You miss the the added bonus of able to see what the seismic responses |
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12:49 | with seismic waves coming in from different and not just, uh, sort |
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12:54 | in our standard two D straight line of what raise and ways will raise |
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13:01 | waves will dio when they reflect and refract through sections of rock. But |
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13:08 | , so a lot of money is there because a lot of money is |
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13:11 | there. Uh, term we used use is it was very sexy to |
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13:16 | a an exploration geologist because that's where the money Waas and and of |
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13:24 | uh, as such, um, lot of effort went into it. |
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13:29 | lot of money went into it. if we go back to here, |
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13:34 | working in production geology, we're actually as close as they could at the |
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13:41 | . And if you can imagine even though the engineers in the past |
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13:44 | have been ignoring this and from uh, this type of information down |
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13:53 | , the production geologists actually had their on more well, bores more |
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14:01 | more sidewall cores. In some enlightened like Norway, uh, they force |
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14:09 | to core every single reservoir you So they had a lot of geological |
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14:17 | stored in that country. I don't if they've tossed it like everybody |
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14:21 | but but it really helps. when you're when you're doing geology and |
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14:31 | you actually are down at this end you have a lot of, well |
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14:35 | , you have a lot of core sidewall core and log data toe |
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14:40 | You actually evaluate the geology with more a hands on approach, and then |
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14:46 | you integrate it with those big pictures you get from seismic, the larger |
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14:51 | pictures, you can get a really understanding of the reservoir and the configuration |
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14:59 | the seals and and all the different , like false that affect seals. |
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15:06 | , that sort of thing through the of integrating all of this type of |
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15:11 | with seismic data. And so that's what happens when we when we move |
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15:17 | Thio the lower end or the or more detailed end of the value chain |
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15:25 | with unconventional. One of the unfortunate that I've seen is that a lot |
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15:32 | geologists become geo steers and the mayor not get to use a lot of |
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15:37 | they know. But I do. do know that when you are your |
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15:43 | steering of your a better geologist, gonna be coming up with better |
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15:49 | Thio understand some of the nuances that be there when you're looking at the |
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15:57 | logs and the other geo steering tools people used to line things up because |
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16:02 | have a better understanding of what types heterogeneity ease that wellbore might be |
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16:08 | even though in the past, petroleum engineers looked at jail is just |
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16:15 | rock type that was homo genius and no, uh, strange things going |
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16:20 | in it. Okay. And of , part a big part of Jesus |
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16:26 | is understanding the layering and the strata architecture of the rocks above that shell |
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16:33 | that you're trying to hit and below , she'll unit and you end up |
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16:40 | very concerned, though with things like total organic carbon. Uh, |
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16:47 | uh, conventional is of course, worry a lot about the charge. |
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16:53 | much do all got in there and lot about permeability. It's the same |
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16:59 | with the unconventional is accepted. You , we have micro ferocity and we |
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17:03 | microbe or actually micro permeability. One the interesting things about Shales is that |
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17:11 | many cases they might actually have more than the sand stones. But the |
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17:16 | , because the pore throats and the air smaller, you have a limited |
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17:23 | . So again, getting back to main concerns of frontier. Ah, |
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17:32 | what Those are, of course. big is it now? We'll go |
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17:36 | this again when we start actually looking more detail at frontier expiration. But |
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17:42 | are the things that are most Obviously, what type of basin is |
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17:47 | where the depo centers in other a depot center, of course, |
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17:52 | where some sort of distributing things like river or a delta distributing sediments will |
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18:01 | it down in certain places in in ways. And you're looking for areas |
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18:07 | , uh, in the case of , where where the coarser grained sand |
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18:13 | , uh, might be getting And, uh, and then you're |
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18:18 | at the types of structures that impact and the overall size of things that |
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18:23 | form traps. Um And so that's of the first things we start looking |
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18:32 | , uh, in the just underneath here in Houston. If you look |
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18:39 | a seismic line, you see a of flat lying beds, and it |
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18:44 | you wonder if there could be any at all. But if you go |
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18:47 | a place that's a little bit more Lee active like the North Sea or |
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18:52 | of the areas off of Alaska in off, um, Brazil and on |
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19:02 | in the Gulf of Mexico, where have salt tectonics impacting structures and stuff |
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19:09 | that, we start to get So we see structure in that size |
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19:14 | and, uh, and then, course, one of the first things |
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19:16 | have to figure out is really doesn't organic rich deposits, and, |
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19:24 | and if it does, how deep they been buried. And so, |
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19:32 | , probably in the late seventies, eighties, a lot of oil companies |
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19:38 | went around the world and identified all major basins. I pointed this |
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19:44 | Thio, uh, somebody from a that this had been done a long |
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19:49 | ago because they got excited about this . They started to call super |
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19:55 | And I pointed out that, you , we we kind of already know |
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19:57 | the in quote super basins are, that's what we've been studying forever. |
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20:04 | , uh, it's amazing and industry we come up with these buzzwords that |
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20:08 | us get excited about things that we've doing forever, but that that's |
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20:13 | But but again, in frontier let's take the Atlantic Coast, the |
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20:20 | Atlantic again it's a good example of . And, uh, one of |
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20:27 | first things they worried about was Do they have organic rich deposits? |
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20:33 | how deep is this and why would be worried about, uh, if |
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20:38 | is still there? I can't see . But if someone's there, could |
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20:42 | answer to me why it's important to deeply buried organics? Because I know |
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20:48 | of you I think most of you just had geochemistry. Thermal maturity? |
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20:56 | . If if it's not deep it's not going to be cooked. |
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21:01 | , uh, if I mean a good example of a place that has |
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21:08 | of organics is the Green River and that's where the oil shale comes |
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21:17 | and why we have to call that shale and the stuff we find unconventional |
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21:22 | shale oil because we're already using oil for undercooked organics that, with a |
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21:31 | bit of heat in a little bit retorting, could be turned into liquid |
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21:38 | . So this is really, really . And if we were, contrast |
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21:42 | Atlantic coastal plain to the Gulf coastal . If you know anything about the |
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21:50 | AFI of both of these, what's first thing that you realize about the |
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21:54 | coastal plain versus the Gulf coastal shallow bedrock, the bedrocks pretty close |
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22:05 | or the or the basements Pretty close the surface is this. Is this |
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22:09 | fellow that went to school in South ? Yeah, exactly. Yeah. |
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22:16 | it tricks anybody that's worked in the of Mexico, but the sedimentary wedge |
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22:22 | the coastal plain itself is actually very thin. You have to go |
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22:27 | off shore to get a thick, wedge, and so that bothered people |
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22:32 | lot. And, of course, of the first things Exxon Mobil did |
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22:37 | long time ago was drill a well on the Outer banks of North Carolina |
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22:44 | they kind of stick out into the Ocean and they got some pretty decent |
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22:49 | there. But you're looking at something 7000 ft at the most. Whereas |
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22:57 | the Gulf of Mexico, of uh, if you drilled a well |
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23:02 | , it might be very difficult to hit igneous and metamorphic rocks. |
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23:08 | um, so the sentimentally wedge in Gulf of Mexico is much, much |
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23:14 | . Uh, sediment. Infill and has been much more significant than on |
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23:19 | East Coast. The the underlying basement been much more stable on the East |
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23:26 | . Thin, of course, in Gulf Coast, which has been subsiding |
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23:29 | it's cooled over the millions of It's all developed of the East |
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23:36 | is is cooling just a little bit and subsiding a lot slower than the |
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23:42 | of Mexico and sediment load has a bit to do with that as |
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23:46 | Okay, so So the first thing we start looking for, of |
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23:50 | is have the organics been cooked? then, of course, all of |
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23:54 | things are important to I remember some projects probably 10 years ago where some |
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24:02 | got really excited because they they were really sharply define a really nice trapping |
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24:13 | . But the thing was very It might have had if it was |
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24:18 | 100% ferocity. Thes traps would have had less than 10,000 barrels of |
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24:26 | They were just really small structures. one of the things that you you |
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24:33 | to look for, of course, is there enough of a resource to |
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24:40 | spend the money it takes to drill well and, uh, and pull |
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24:45 | resource out and make a profit? . Uh, actually producing more than |
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24:56 | a little bit. And and that actually one of the most significant differences |
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25:03 | conventional and unconventional is in conventional. looking for those really high permeability, |
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25:11 | porosity ah, fields that will drain awful lot of oil with one well |
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25:19 | . And when you when you put unconventional well, a horizontal well in |
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25:25 | ground, you're the surface area and of it's sort of a false sense |
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25:33 | reach. The acreage that you might able to reach seems a lot |
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25:39 | but the total volume of that acreage much, much smaller in conventional |
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25:45 | And that's why you have to keep a well and drain that limited volume |
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25:51 | that large area that you have of and gas. Because the pores as |
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25:58 | process as you have the pores air small. The permeability reach is limited |
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26:05 | so you don't usually drain as nearly much volume. Aziz, you could |
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26:11 | in this in a smaller cross sectional in a in a conventional wealth. |
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26:19 | so that size of the difference in size of the volume is significant in |
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26:23 | of where you can put that pressure between the wellbore and the formation to |
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26:30 | the oil and gas to flow. , so here again, based on |
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26:36 | those things that we look at, , this is, um, whenever |
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26:43 | put this figure one, whatever down , usually that means that it came |
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26:49 | of glue, ISS and Swarbrick, I don't have it quoted down |
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26:54 | But this is, Ah, a type basin, we call it, |
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27:00 | this looks very much like the North and other rift basins around the |
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27:07 | and we can see through time there's , may be sentimentally rocks was what |
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27:15 | is showing that predated the rift So it's pre rift, and what's |
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27:21 | on in here would be sin rift then post rift sediments up here and |
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27:28 | these little symbols air showing you Here's where reservoir rocks could be formed |
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27:35 | here's where source rocks could be Uh, once you have, |
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27:41 | larger ocean basin and you have these fight of plankton falling all right to |
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27:46 | sea floor, and then you have build up of sediments on top of |
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27:50 | that buries it. And so you all these things that we're looking for |
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27:54 | that list that I showed you. have something big. We have trapping |
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28:00 | . We have seals, which they're cap rock here because otherwise they'd have |
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28:06 | s and they have seals and Uh, so they're calling it. |
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28:12 | seal is the cap rock. It's really a cap rock, but it's |
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28:16 | seal. And, uh and here can see, uh, during pre |
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28:25 | during sin riff post rift and and , uh, this is post rift |
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28:33 | you have thermal cooling of the basin starts to sag like this. Because |
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28:39 | the drifting is ongoing, this is up in the air and we'll talk |
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28:46 | that, uh, in section five electrified. So, of course, |
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28:54 | conditions to convert resource is to a . You're gonna have to come up |
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28:59 | money. You're gonna have to have . You're gonna have have to have |
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29:05 | . And what else are you going need? Okay, Anybody have any |
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29:18 | of what else you're going to need prospect exactly. You're gonna eventually have |
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29:25 | thio have all that data that we talking about and you're gonna have Thio |
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29:32 | able to do all the things that and geophysicists do but put this in |
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29:37 | because a lot of times, as we're doing the and down here, |
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29:44 | and we need to find all these that we were talking about that air |
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29:48 | for frontier exploration, and, at the same time, we have |
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29:54 | remember that just because we find something looks really good Ah, these things |
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30:01 | the economics of of what we're gonna be doing. And so, at |
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30:09 | frontier level, in the sort of new ventures level, companies spend a |
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30:14 | of time, uh, looking at access can I get access to |
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30:19 | And there's there's a couple of different some, some countries and some states |
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30:26 | whatever, wherever you're trying to may have excessive rules and regulations and |
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30:33 | . Uh, some places that you want to operate have unstable governments, |
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30:40 | there may be civil wars going on that sort of thing, um, |
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30:45 | you could have a place where there any civil wars in the government's unstable |
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30:50 | on. And anyway, I and, uh, then another thing |
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30:55 | , is there any kind of infrastructure ? And, uh, you |
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30:59 | in a very, very frontier you kind of have to figure |
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31:03 | you know, if I actually found , how how am I going to |
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31:07 | that oil out of there? uh, but the up front end |
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31:12 | all of this lot of people in corporation are going to be trying to |
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31:17 | out, you know, for of its in Indonesia or something, |
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31:21 | Papua New Guinea. Do I have to build, uh, docks and |
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31:27 | , in some cases, ship channels get to get chips in their |
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31:33 | pull some of these resource is And then, of course, how |
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31:38 | is it in? The bigger it , the more capital you can |
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31:42 | And and of course, that's a big part of the equation in the |
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31:46 | beginning and in in the discussions that have when it comes to frontier |
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31:54 | Okay, so when we move on what we do and expiration and exploitation |
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32:02 | opposed to senses, strict frontier Ah, we figured out that we |
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32:10 | all those elements in frontier and we're to look for, uh, these |
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32:18 | and coming back to this diagram. know there's a lot of structure |
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32:24 | We know there's big, big areas volumes that might have reservoirs, but |
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32:29 | we have to kind of start looking each of these reservoirs individually and each |
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32:35 | these petroleum systems as we call them . Like what? What is the |
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32:40 | system here? What's the petroleum system ? So we have to start looking |
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32:45 | it in more detail. And here we're trying to do is develop |
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32:51 | uh, structures with optimistic and pessimistic on that sort of thing. And |
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32:58 | really trying to come up with what call prospects here. Here. We're |
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33:05 | grossly. You know, where could be prospects? But when we get |
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33:11 | expiration, we're trying to, to develop prospects in and identify prospects |
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33:20 | certain elements to them, like what actually the reservoir Iraq. What is |
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33:26 | about this part of the basin that us that we're going to get sentiments |
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33:35 | more likely than over here, that of thing? In other words, |
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33:40 | all my play elements going to come and let me just ask all of |
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33:46 | because I think some of you started semester some of you. But you're |
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33:51 | working in industry. Why would someone at a large scale seismic section consider |
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34:01 | would be a reservoir over here as to right here? Mhm. Because |
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34:14 | the like. We were small. cyclical structure. Okay, so what |
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34:22 | this What is this? These sets lines reflecting down lap into the basement |
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34:31 | down lap into the basement. Here's a down lap. Right. But |
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34:36 | what you have is, uh, better word to use is you see |
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34:41 | gradation. You see pro gradation of across the shelf. And this |
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34:49 | Nation of Sediments. Ah, uh, reflects the infill of a |
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34:59 | with sediments of varying sizes. But we see, uh, these things |
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35:07 | we call actually Klein of forms, are these kind of forms? Usually |
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35:12 | a geology geological sense. Like if you a za geologist and you just |
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35:23 | at this structure first thing, these air sediments, these air sediments |
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35:31 | air pro grading out in this right. What's going on inside each |
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35:39 | of these? Um, these these reflections or boundaries are the klein |
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35:45 | forms. But the rocks between the of forms Klein of films. |
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35:51 | um, these air, the Klein them is means things. So |
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35:57 | I like to call him klein of . So these kind of things here |
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36:02 | this. This layer of rocks right . What would be, um, |
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36:08 | sedimentary composition? Just along here. , if I see something that looks |
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36:16 | this, it's probably gonna be And if it's ringing like crazy, |
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36:21 | probably gonna be basement. What if see layered rocks like this? And |
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36:26 | , this first thing I know there's rocks here, and I also know |
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36:32 | been structurally deformed, but here you see structural deformation. The tilting here |
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36:40 | structural deformation. It's pro gradation. what are what are these Plano thumbs |
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36:47 | to be filled with from, the top to the bottom? What |
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36:51 | we anticipate as a geologist? Especially that's had sequenced fatigue? Ra |
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36:56 | What can we anticipate might be in Klein? Oh, Finney, you |
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37:04 | alternating sandstone and shale beds, And but, you know, that's |
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37:12 | . And you know some of these subtle things they're really obvious. And |
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37:19 | , But, you know, we to think about, um uh and |
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37:23 | what happens is if we were to faces on this, the coarse grain |
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37:30 | would be upheaval and the and then start getting more silkier less sand and |
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37:37 | silty as we come down here. then we started getting more clay and |
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37:40 | as we come down the Klein a . And if you see it in |
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37:46 | later lectures, I'll actually show this you. But But when I see |
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37:50 | like this, I know that across Ah, that there should be |
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37:57 | And down here there's going to be . And but that's why they put |
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38:02 | reservoir somewhere in this climate form ah, this may seem really |
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38:10 | But when when we have seismic lines look like this. And this, |
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38:18 | , one thing we don't know about sure is that there's sand in here |
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38:24 | the time with three D seismic. we can kind of sort that |
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38:29 | Uh, in some places, like North Sea, where chalk is still |
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38:34 | major absorb er of energy, it be difficult to image down in the |
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38:39 | below the chalks eso. Sometimes that even help. But if we can |
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38:45 | Clinton forms, for example, if could identify client forms in these layers |
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38:50 | rocks, one of the things decline forms tell us is we have |
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38:55 | procreation. And when we know we procreation, we know at the upper |
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39:01 | of it we're gonna have coarse grained and, uh, at the lower |
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39:06 | of it, we're going to have grain sand. So it's kind of |
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39:10 | , uh, a strata graphic and of a reservoir rock just above something |
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39:18 | could end up being a source And you can see here there's source |
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39:22 | here, and there's Reservoir rock there a cap over top of it. |
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39:27 | in here, we're going to get of sources down here. We'll get |
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39:31 | . But up here, we're gonna a reservoir rock forming at the tops |
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39:35 | that. In other words, each one of these climate forms is |
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39:39 | be course up here and finer and it's going to integrate from that |
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39:44 | defined as we come down there. that's just the way pro gradation |
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39:49 | Delta builds out the heavy sediments, out first, and then the finer |
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39:54 | finer and have finally it's mostly pelagic and phytoplankton being heavy plastic sediments |
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40:02 | phytoplankton being deposited out here. So the fact, uh, from A |
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40:08 | D seismic lines. Seeing climate forms us hey, there could be reservoir |
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40:15 | . But then the next thing we to do is eyes understand the thickness |
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40:21 | the section. The other elements of frontier are important. But as we |
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40:25 | into exploration, we're trying to look what makes this element good. What |
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40:32 | make this element good? And down we have another reservoir. What would |
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40:42 | these sedimentary rocks a particularly good reservoir opposed to, say, this one |
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40:50 | that one? And in fact, aren't these if that ISS So those |
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40:56 | the kinds when we start doing we're not just looking for the big |
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41:01 | of Are there these elements? We're to look at where all of these |
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41:08 | come together. And so if I a source, if I have something |
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41:14 | looks like a reservoir rock, how I migrate source material? I have |
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41:22 | kitchen. Do I have migration, pathways to get to that reservoir, |
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41:26 | charge that reservoir. And that's what start looking at an expiration in frontier |
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41:32 | . We're trying to look and see we have these kinds of things. |
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41:35 | we have these kinds of things. while we're at it here, we |
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41:39 | a reservoir. I point out its brain. What? What geological process |
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41:45 | have caused something like this to end being, Ah, Prospect of Reservoir |
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42:04 | . As a geologist, as geologist geoscientist? Um, why would I |
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42:11 | a wedge like this in a Excuse me? Like separate position. |
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42:26 | what type of deposition? Mhm. , it is sin rift, but |
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42:33 | a little bit more specific. I , this is this is a |
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42:38 | but this this represents program nation obvious gradation. Okay, we've got climate |
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42:46 | building out into a basin that's dead . What this is this is is |
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42:56 | to, but again, it's a . But what is this cartoon? |
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43:01 | would what would that have to Uh, mind you, all of |
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43:08 | , this would be up higher when is going on and because this is |
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43:16 | a rift might look like now. that's after we've had thermal contraction of |
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43:21 | magma that caused the rift in the place. When the rift ing is |
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43:25 | on, this is all up. this and the new layers Uh, |
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43:32 | section of crust or moving in that . And in that direction, they're |
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43:38 | off the flanks in either direction. during this period of time, which |
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43:45 | sin riff. What's happening here? do you think could be happening? |
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43:52 | that like a classic wedge that gets ? It is a classic wedge, |
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43:59 | what kind of plastic? Which I'm say, Yeah, submarine fan. |
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44:10 | , but not quite. Yes, what this is right here. This |
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44:15 | a submarine fan. And and I since you came up with the idea |
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44:21 | fan. That's what this little beauty in a cartoon because we're way off |
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44:30 | . And here is the bottom of basin at that. At this point |
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44:34 | time, Uh, that's the bottom the basin, which might not have |
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44:41 | quite a deep when it was actually deposited, because we've had this much |
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44:48 | occur and we're And as all of is going on, we were getting |
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44:53 | contraction and sinking along this axis. , uh, what's going on here |
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45:01 | that when this happens, these would popped up in the air and, |
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45:08 | , this would be like the rims a Rift Valley like, say, |
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45:11 | Turkana or the Rift East African Rift . You'd have these mountain ranges along |
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45:17 | edge of the rift, and sediments be eroding and pouring down into whatever |
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45:24 | of the basin had formed at that . Of course, this is going |
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45:28 | be up uplifted a little bit when happened, but you're still gonna have |
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45:32 | rift in the middle. Uh, the East African riffs and sediments they're |
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45:37 | be dumping into it off of the fault blocks around it on either |
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45:44 | and they're going to be forming. uh, large, uh, fan |
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45:53 | . We sometimes call these things on large fan Delta right here is going |
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46:00 | be something like the brace Sands that off in the Jurassic. So it's |
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46:08 | like in a in, uh, some cases, it may be on |
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46:12 | surface, and this could actually be alluvial fan coming off of a false |
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46:17 | , but a zit turns out there a bit of a Rift lake going |
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46:24 | and actually had some marine incursion into at that time. Eso it wasn't |
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46:30 | like anymore. It was a a early Rift Basin and you had |
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46:36 | it pouring off. And you can here there's an uplifted block here |
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46:41 | and this would be more of the when that formed. Uh, for |
|
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46:46 | , if we remove all of this here and go back to the time |
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46:50 | this is sticking up in the thes air, huge mountain ranges |
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46:55 | uh, and sediment is being eroded the top of these things, you |
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47:00 | see that it's thinning in that direction and it's pouring off into these |
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47:06 | And the brace sands in the North are exactly like this, right on |
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47:10 | edge of a rift fault block that the boundaries off the north of the |
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47:18 | robin right now. And the South Robin, uh, also. And |
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47:26 | have actually the junction of central grabbing the South Viking. Robin, you |
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47:31 | these things pouring off there. So have these huge Jurassic, um, |
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47:36 | not submarine fans like this, but fans that are more like fan Delta's |
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47:42 | they're coming into, uh, ocean salt water masses rather than just into |
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47:50 | alluvial plain. Uh, and so not just alluvial fans coming off that |
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47:56 | see in rift blocks right now, , in different parts of the Western |
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48:01 | . S. Okay, so that's of it. So what's interesting about |
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48:08 | little cartoon is it tells you an lot about all these different ways that |
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48:14 | can develop reservoirs. We can develop and we can develop sources and and |
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48:23 | mhm. This would be a different concept than this prospect concept. And |
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48:32 | would be a different ah petroleum system reservoir concept, then that one this |
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48:39 | has to get a charge from a place than that one. This one |
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48:44 | sediments derived from a different place than one. And so these air all |
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48:49 | different elements. But these elements arrive in a petroleum system through different processes |
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48:58 | time through the overall development of the . Which is why we like to |
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49:03 | basins because they this rift system right has an enormous number of petroleum systems |
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49:14 | in it. Because of all the , actually, is the easiest way |
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49:18 | say it to create, uh, instances of these elements of that petroleum |
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49:28 | occurring together, and that's That's one the things that's really incredible. Incredible |
|
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49:33 | rift basins and why we get a of hydrocarbons out of rift basins. |
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49:39 | , so that's what we're doing with and exploitation. Uh, with |
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49:46 | We're trying to see if we have of elements, you know? Is |
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49:50 | big? We have lots of Is it deep? Is this deep |
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49:53 | to actually create a lot of source ? Could this source rock charge that |
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49:58 | , that reservoir? And how would charge this reservoir? And we can |
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50:03 | it in the big picture. But , in frontier and exploitation and |
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50:08 | we try toe put these elements and this would be a prospect |
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50:13 | This would be a prospect concept that be a different prospect concept. And |
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50:19 | once we drill into it, you , that's when we go from |
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50:23 | Excuse me, Exploration, exploitation. we try to figure out okay if |
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50:28 | one here. Is there one over ? If there's one here, is |
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50:33 | one over there? In other we get this prospectively concept in our |
|
|
50:38 | and and we look at the base more detail to figure out if you |
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|
50:44 | , here we have one here. where else are we gonna have? |
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50:48 | can we exploit the space? And on this concept, in more |
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50:54 | because of what we've learned and what blocks, for example, I've hit |
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|
50:59 | fault. Block. What other fault might have been charged the same way |
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|
51:03 | this one is. I just discovered and gas, okay? And that's |
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|
51:08 | we kind of go with exploitation. and then, uh, so you |
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51:15 | have gotten some acreage to drill that prospect. But then, when you |
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51:21 | of shift into exploitation mood, where am I going to find that in |
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51:26 | base? And based on the seismic I have, I don't have any |
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51:29 | wells there, But based on the , where else can I move this |
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51:37 | concept of what a basin is? me. What a petroleum system is |
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|
51:44 | that area, okay. And so as we get ready to drill |
|
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51:51 | uh, exploratory wells, we look a lot of these different things. |
|
|
51:56 | again, I like to add these that aren't geologic because as geologist, |
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|
52:05 | not trying to discover just oil we're just trying to discover where our reservoir |
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52:13 | could be, although in frontier, those elements aren't there, there's no |
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52:20 | in looking any further. So that's we do that in the beginning. |
|
|
52:25 | once we start trying to tap into , all these other things that I |
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52:31 | talking about become important. Where do actually locate the will? What's going |
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|
52:37 | with all these things? Uh, guess many of you know that Mobile |
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|
52:43 | , for example, is a is an area that has some major gas |
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52:49 | , uh, in it. And long do you think it might have |
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|
52:55 | Mobile was actually the first a company drill, uh, there. And |
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53:02 | long do you think it took Uh huh. From getting a |
|
|
53:08 | And they purchased acreage and they started , well, sites. But how |
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|
53:17 | do you think it took them? of environmental concerns to to get the |
|
|
53:24 | to actually drill on that acreage that had purchased. Anybody have any rough |
|
|
53:38 | ? It's anybody's still there. Was it years? Was it |
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|
53:45 | Yes, it was years, and was about 10 years. It's, |
|
|
53:52 | think, Actually, it was nine in so many months before the |
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|
53:57 | uh, approved it. And uh and so ah, lot of |
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|
54:03 | went into the frontier part of a lot of seismic went into |
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|
54:08 | Uh, they actually had thio pay the lease upfront Bonus. They did |
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|
54:14 | an extension on the the time of least. Normally, you have a |
|
|
54:18 | amount of time Thio drill and find . And but that was extended. |
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|
54:25 | it took It took nine years. why? Because Mobile Bay is ah |
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|
54:30 | an area. Uh, you that's environmentally significant for ocean health or |
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|
54:38 | Gulf of Mexico is health because as most folks now and I'm assuming that |
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|
54:44 | do, because all of you are science majors, uh, and maybe |
|
|
54:50 | a lot of science courses in high , but the estuaries, like Mobile |
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|
54:57 | or where ah lot of the life the ocean starts out and you don't |
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|
55:02 | to damage sort of the birthing spot many, many things that actually end |
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|
55:08 | contributing to the health of a notion terms of organic productivity. So, |
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|
55:15 | , that's why that took so And of course, safety is always |
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55:19 | . And but then you have to thinking about all of these things, |
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|
55:24 | , because, uh, if you're shore, there's a way to do |
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|
55:28 | . If you're offshore, there's a to do it. If you're sitting |
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55:31 | in front of an environmentally sensitive you have to be really careful how |
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|
55:39 | dispose of waste. And all of adds to the cost. And |
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55:44 | as geologists and geophysicists or geoscientists in , we always have to be thinking |
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55:51 | of, you know, if I more of this to deal with, |
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55:55 | I have more of that to deal when I'm a to this stage, |
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56:00 | need to be looking for bigger Resource because the probability of success and getting |
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|
56:11 | that's profitable is impacted by these elements here that have nothing to do with |
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|
56:17 | geology. Okay, so here we , uh, as I was mentioning |
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56:26 | the bigger diagram, because I thought was good, too, to sort |
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56:31 | go from the bigger diagram to the diagram. So when we get the |
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56:35 | and exploitation again, we're looking at prospect level and we might decide this |
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56:43 | the best one. But if we oil and gas here, we might |
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56:48 | exploit that opportunity and try to determine that same opportunity might be here a |
|
|
56:55 | . And so that's pretty much kind the way those three things go. |
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|
57:01 | then, um, then we get . We actually drill a well on |
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|
57:08 | best prospect of its successful we we get a flu to champagne. |
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57:14 | it's not successful, we got a bottle, and this is almost a |
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|
57:18 | as the humor gets in my Uh, because we're not really allowed |
|
|
57:25 | cuss anymore, and I don't know , but humor benefits often from foul |
|
|
57:31 | , but but But anyway, this is a little bit of humor |
|
|
57:36 | , but the other thing is, we hit a fault. And, |
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|
57:41 | , I mentioned this before. if you're yes, you're not drilling |
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|
57:49 | exploration well, but you're drilling in will. You might hit the faults |
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|
57:55 | you might hit you all water but you may never find out. |
|
|
57:58 | oil and gas there. And so the location that I talk about here |
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|
58:06 | . You get it this scale, don't drill. Ah, well, |
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58:10 | here to figure out where that oil contact ISS. You know, if |
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58:14 | drill a well, let's see if all the way out here because then |
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|
58:16 | know it's worth drilling. Let's drill right here, because then we'll get |
|
|
58:22 | well water contact in the seal. you need to do is to get |
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|
58:26 | here and make sure you actually have nice, thick wedge of sediments that |
|
|
58:31 | charged with oil and gas. So exploration well is going to be different |
|
|
58:36 | those appraisal wells and some appraisal You might get lucky. And, |
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|
58:43 | example, maybe you think about what contact is up here and you drill |
|
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58:48 | here and you get more sex section there and you can turn that into |
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|
58:52 | producing. Well, the dog can Can I make a comment? So |
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|
58:58 | , I think, I think, because of, um, cash |
|
|
59:04 | like you're saying we almost jump that are in exploration, but we want |
|
|
59:10 | appraisal well, right. We want get the two coins, and and |
|
|
59:16 | sometimes it's frustrating because it's a geological . it's proven the play, but |
|
|
59:22 | we gotta push back because it's not course big enough for yeah, of |
|
|
59:27 | . For the company, That's uh it doesn't make profit for |
|
|
59:31 | But, uh, like you're saying is not exploration anymore. You're |
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|
59:36 | But if I If I may, that's really sort of a false |
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|
59:42 | because on their part, because when drill a well right through here, |
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|
59:51 | am I going to figure out? going to see that oil water contact |
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|
59:55 | , just like I will out Onley here. I will know what's |
|
|
59:59 | it. And and maybe we think oil water contact could be here, |
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60:07 | the oil water contact could be And if the well water contact is |
|
|
60:12 | , we're probably not gonna wanna I to do any more drilling. But |
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|
60:16 | I drill through this, I find oil on top of it, and |
|
|
60:21 | thing called in oil water contact is be underneath it. So I just |
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|
60:25 | to make sure I go all the . And of course, of in |
|
|
60:29 | drilling plan to save money, they go this far. But it's still |
|
|
60:35 | oil, water contact. It may down here, and that's going to |
|
|
60:39 | excite them. If you're still above oil water contact and s o |
|
|
60:48 | if you if you go for the lode, you confined some of these |
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|
60:52 | . Mhm. Just by going a bit deeper, we don't have one |
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|
60:58 | . Right? But if you had fault over here that you were worried |
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61:01 | sentiments like that, you might, you could also hit a fault or |
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61:05 | trap. Excuse me. And in , water contact. Where did you |
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61:09 | in here like this? You do the fault, but make sure, |
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61:14 | , the whole sections not faulted out it would be right here. Do |
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61:21 | think that, like, kind of follow up? Do you think that |
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61:24 | companies, when you know, it's hard to recommend drilling a well, |
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61:28 | for the sake of science? But you think that have you or have |
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61:30 | seen that For the most part, have benefit benefited for doing something like |
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61:35 | where, unlike in today's time, so hard to convince people to drill |
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61:39 | for the sake of collecting data, know. Oh, yeah, But |
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61:42 | here, you for that first? , you might have. You have |
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61:47 | gonna have some indication of where that water contact should be. And if |
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61:52 | not sure, if you if you it. But the the height of |
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62:00 | hydrocarbon column is going to be limited the strength of the seal above |
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62:06 | And I think Steve talked about that little bit, and I'll be talking |
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62:11 | that. But some people have often in the past. Before they thought |
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62:17 | how seals leak in fracture from hydrocarbon , they might have just automatically put |
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62:26 | it way down here. And with little bit of calculation, you can |
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62:32 | out that that the buoyancy of a that high is probably going to exceed |
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62:37 | strength of the seals in that particular . And that's another thing that you |
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62:43 | do, and especially if you If you're in exploitation and you have |
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62:48 | fault block like this somewhere else, it's in the same reservoir around the |
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62:53 | depth, should be in the same regimes more or less than that sort |
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62:58 | thing on you. Haven't you have idea The strength of the seals. |
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63:04 | , you can get a better idea where that oil water contact should |
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63:09 | And drilling straight through like this for expiration. Well, is basically trying |
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63:17 | find the most important thing that you drill with that first well, is |
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63:24 | oil section. And that's what you're for is the oil section. If |
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63:31 | if you miss it, you you've you've wasted a whole well and |
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63:36 | nothing. And, uh, if just come in over here, you're |
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63:42 | have a thin section be worried you know, does it shell |
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63:45 | up dip. And and it depends the structure and the deposition. I'll |
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63:51 | and the sequence photography and where you in a client a form, for |
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63:55 | , as to whether it would be dipper down dip. But all those |
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63:59 | you have to take into consideration. if you come in and drill |
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64:02 | you're gonna figure that out just from straight through there. And that's that's |
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64:09 | you know, your first of all to be here. We're here and |
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64:14 | right on this fault to figure out that fault boundary is and not right |
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64:18 | back here to figure out where the closure on the oil water contact might |
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64:26 | . And, of course, with two D seismic, you can figure |
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64:29 | where the structural closures might be. that shouldn't be something that you're drilling |
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64:35 | when you drill that first. um, you really should be looking |
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64:40 | the bull's eye, and I don't how to say it any any any |
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64:45 | . Um, do not. You that first dark that you throw needs |
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64:50 | be in the bull's eye. And you think the sweetest, thickest section |
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64:56 | , that's where you need to And when you're doing unconventional, that's |
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65:00 | what you need to dio. You go journaling out in the middle of |
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65:05 | with no idea of what the what micro permeability might be like. And |
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65:14 | , of course, with unconventional, also looking for, uh, water |
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65:19 | there because the more water that's in , the more more of that terrible |
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65:25 | about permeability you'll be ableto capture into fractures. Okay, so I hope |
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65:36 | know if people are getting in the about drilling here vs there that's that |
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65:41 | be why they're missing a lot of . And, uh, in the |
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65:47 | Sea that I meant one thing that mentioned, they danced around it like |
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65:53 | . And, uh, there was fault over here, and there was |
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65:56 | million barrels of oil in here the fall. Down there, there was |
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66:01 | . There was 110 up here, there was lots of oil and gas |
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66:06 | here on the other side. They figure out whether there was sand here |
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66:11 | they kept drilling here and here. they kept missing the sand for reasons |
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66:15 | than the ah, there wasn't anything the middle. He if you miss |
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66:22 | bull's eye, you might not even . Uh huh. Where these boundaries |
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66:27 | actually going to be? Because you drill a well over here and you |
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66:31 | drill a well over here, and what they were doing. Okay, |
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66:37 | So when we get Thio appraisal, when we really wanna We really want |
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66:41 | figure out your very second Well, you know, there's something significant with |
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66:46 | first Well, then you do have go out and drill the 2nd and |
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66:50 | . Well, now, if you're at something really tiny in the first |
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66:55 | , you still need to figure out that hydrocarbon column looks like. And |
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67:02 | only way to do that the way figure out the absolute height of that |
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67:07 | is to drill right through here. it can only be so high because |
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67:12 | seals can only hold so much oil . Okay. And then, |
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67:24 | eso you do do the rest of things. And, uh and so |
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67:29 | appraisal, you start drilling these and here you find out your past |
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67:33 | all water contact, you've drilled these and you figured out there's false separating |
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67:39 | . And what you find out a of times with appraisal wells is that |
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67:45 | reservoir that you once thought was this is actually more compartmentalized. |
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67:54 | then you thought it waas And I the idea of trying to figure out |
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68:00 | that compartmentalization is in the beginning. if you drill this well, you |
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68:05 | never come. If that's your number . Well, you may never come |
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68:08 | to this at all, and there be a significant economically recoverable, |
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68:14 | reserve in here that you're going to if you drill this well first. |
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68:19 | in that one second, you may do it. You drill this |
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68:23 | First, you may not ever go and look at that resource. But |
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68:28 | where it looks like it's most perspective well, you drilling when you drill |
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68:33 | well, you should be able to out where this is right here. |
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68:37 | only thing that you're actually doing when drill out here it's not finding the |
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68:41 | water contact. But when you drill here, you're trying to figure |
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68:46 | um, if there's some sort of between this well and that oil water |
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68:53 | out here and if the strata graphic the structural closure that you think is |
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68:57 | is really there or not. So figuring different things out when you start |
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69:01 | as appraisal wells. In other you might have from your seismic you |
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69:06 | think the closures like way over here this. When you drill that |
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69:10 | you'll find out that's not true. appraisal Wells help you figure out the |
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69:16 | extent. But they also help you out how broken up that resource |
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69:21 | So this target should be something that very perspective in the first place. |
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69:26 | want to do something like a bull's in the sweet spot and try to |
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69:31 | out what but that hydrocarbon column really like not by looking at the |
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69:39 | but by looking at the middle of and, uh and then also what |
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69:45 | of compartmentalization it is, because when do production and development, uh, |
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69:50 | a field like this, it's gonna a whole lot different than something That's |
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69:54 | simple, where you can put a pipes in there and drain it without |
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69:58 | effort. Okay, so when we to development and production, of |
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70:06 | moving product becomes important. You may infrastructure, but you might realize you've |
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70:12 | this really big field and you need get more pipelines, which is happening |
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70:17 | the Permian Basin right now. uh, you want to figure out |
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70:25 | you know, how much of a do I need to put on |
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70:29 | On? That show could have something do with how much product you can |
|
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70:35 | . There may be limitations in the . There may be, uh, |
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70:40 | in the price, and you might shut it in when something like that |
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70:45 | , if you can again. If drilling unconventional wells, you have to |
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70:50 | drilling and you have to keep And you have to keep that cash |
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70:53 | rolling, or you're gonna have have with cash flow. And how many |
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71:01 | does it take? And then you to start thinking about things like reservoir |
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71:06 | A TSA um, point, because as geologists, we know we |
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71:13 | these structural heterogeneity ease that you see this diagram. But then you may |
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71:18 | deposition of heterogeneity ease in this in whole oil column that affect the rate |
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71:26 | flow in different directions. In other , there's anti Satrapi to the flow |
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71:34 | and there are a lot of different that we have to look at. |
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71:38 | , particularly we're looking at the strata architecture of the of the sediments that |
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71:43 | up that. That column if it's sandstone or a silty sand stuff, |
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71:52 | , and and again, when we into production, Andi, we're gonna |
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72:00 | looking at all of this a little closer e don't want to give it |
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72:04 | away, but again, we're looking different details. But here you can |
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72:07 | we have injection wells Thio, try help things out here. You have |
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72:13 | quality sands coming in through here, it could actually extend extend across |
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72:18 | In other words, you can have sorts of issues with faces and what |
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72:23 | that start compounding things. And before started putting in, inject an injection |
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72:29 | like, for example, one here probably not going to do you a |
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72:31 | lot of good. You need to , Ah, the overall structure and |
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72:40 | . All these things that we used define rock types start to become |
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72:46 | And what's really odd about this is doing really good production takes a lot |
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72:53 | geological input, and, historically, za petroleum or reservoir geologists would be |
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73:02 | at. This is a big tank the ground, uh, even though |
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73:07 | lots of wells and there's lots of really geological data. A lot of |
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73:10 | used to get ignored. Nowadays, not being ignored like it was in |
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73:15 | past. Now we're we're spending a of time in development and production to |
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73:21 | better characterize these reservoirs and look at flow characteristics and the heterogeneity. Is |
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73:30 | occur within these sand stones? as geologists, we know that sand |
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73:36 | and Shales air not homogeneous. so So basically, you get to |
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73:45 | appraisal thing, you start to delineate . Then you start to develop again |
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73:50 | and you do that. Reservoir management recovery. When I was working in |
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73:56 | Marsh Island 1 28 I was Um, South Marcelin 1 28 is |
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74:05 | still the most productive three square mile in the entire Gulf of Mexico. |
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74:12 | , it's interesting field that probably has this point in time. 30 or |
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74:17 | pay zones. Hey, layers uh but also, I don't know |
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74:24 | I mentioned this already, but they had, um, strata graphic traps |
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74:31 | that all the production geologists and exploration overlooked. They were actually down dip |
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74:37 | some of their oil water context, we were able actually to find those |
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74:40 | start producing those. So when I working on that field, I actually |
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74:45 | doing we were working in an area we were trying to do water |
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74:51 | So we're working at this scale. were doing, uh, appraisal |
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74:57 | trying to figure out what the downward of some of the mass of sandstone |
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75:02 | were with with well over 20% ferocity the same time I was looking at |
|
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75:12 | . Um, if this petroleum system strata graphic traps, where could they |
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75:17 | be? And how could we possibly those and drill does. And so |
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75:22 | found a lot of stuff that was down dip in a strata graphic trap |
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75:28 | the same fault block of something that a higher oil water contact for, |
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75:34 | , sandstone that was isolated from this graphic trap. So it was It |
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75:39 | a really, uh, really good for someone starting out in production, |
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75:45 | and the oil industry to actually learn awful lot. And, of |
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75:49 | at the same time, I had field these Cameron 81 that had a |
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75:54 | gas blowout with 100 million cubic feet gas going to blue sky, |
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76:02 | somewhere around five months, and, , that really got me into another |
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76:07 | of what it's like to be in oil company. All over the same |
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76:12 | of time and in a relatively short of time. So it was a |
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76:15 | interesting time in my life. So again, you know, what |
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76:21 | the types of data? You're petroleum . You're always talking about this kind |
|
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76:26 | stuff. But we're looking for the porosity, The permeability. Ah, |
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76:33 | , what kind of, uh, or barriers do I have in a |
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76:37 | direction? In other words, toe flow. Ah, vertical barrier creates |
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76:44 | flow. A, um um let , uh in other words, if |
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76:53 | have variability in this direction in other , in a layer that's like this |
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76:57 | a layer that's like that it creates , uh, avenues. And if |
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77:04 | have something, uh, that separates this way like a vertical fault that |
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|
77:14 | flow in a vertical direction. So configuration of the layers could be, |
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77:20 | ah. Little bit different than actually way the barriers actually are. We're |
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77:25 | looking for total oil in place, , by, um, zeroing out |
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77:33 | rock space and the fluids, the space, and we're trying to figure |
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77:38 | what the actual recoverable reserves are and of course, the A P I |
|
|
77:44 | can have a lot to do with flow conditions. For example, when |
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|
77:48 | found two billion barrels in place in South China Sea, the luau structure |
|
|
77:57 | , the A p i gravity we really low ap I gravity. But |
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78:02 | viscosity of that particular oil was a lower for that particular gravity of oil |
|
|
78:09 | of bio degradation from bacteria and the that was driving this water drive and |
|
|
78:18 | as it migrated through through the the , that was actually, uh, |
|
|
78:25 | from source to the thing that actually the of viscosity a little bit lower |
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|
78:31 | it should have been for the for density of that particular oil. So |
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|
78:35 | were able to put cheese on It was relatively deep water over 300 |
|
|
78:41 | deep, and they were able to sheets on it, and that was |
|
|
78:46 | heavy oil. With just a little of heating, they were able to |
|
|
78:49 | it the flow. And, of , sometimes this is not a problem |
|
|
78:53 | all, because you have a nice nice uh hi, I a p |
|
|
78:58 | graph and, uh, and of , this water saturation helps you figure |
|
|
79:02 | what those reserves are. And that , which I just mentioned, is |
|
|
79:07 | critically important sometimes in terms of And And you start looking for these |
|
|
79:14 | , Of course, What's gonna happen we bring it thio to the |
|
|
79:20 | Uh, what volumes are we gonna or gain? What's the gas oil |
|
|
79:26 | ? What would the temperature be? bubble point for the dissolved gas, |
|
|
79:35 | and also sometimes the what? Our can also help us figure out other |
|
|
79:41 | in terms of of how this is to flow and drive, and, |
|
|
79:46 | , and that sort of thing. a lot of information goes on into |
|
|
79:49 | . When I worked as a developmental , the reservoir geologists spent a lot |
|
|
79:55 | time working on this, and the would spend more time working on these |
|
|
80:03 | and, uh, trying to get those volumes. Um, actually, |
|
|
80:08 | volumes for this by mapping out the and that sort of thing. So |
|
|
80:14 | are we looking for for unconventional? that kind of went through conventional |
|
|
80:21 | and I mention a little bit of . Well, what would we be |
|
|
80:26 | for once we've got that first well in an unconventional How? Well, |
|
|
80:38 | next Well, right. Yeah, gonna be looking for that. So |
|
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80:43 | already know where the source and reservoir . So obviously Ah, lot of |
|
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80:52 | where we are, we've drilled through source rocks looking for conventional resource |
|
|
80:57 | and so we're already looking at a that has relatively speaking for that whole |
|
|
81:03 | whole source rock with probably were some the best process and permeability, or |
|
|
81:09 | , And we saw that because we might have had shows coming out of |
|
|
81:14 | shales when he drilled for those conventional . But other things that we start |
|
|
81:20 | for, you know, we could some of this with our seismic |
|
|
81:26 | but we're looking for, uh, know which rocks are susceptible to |
|
|
81:32 | Which ones aren't where the primary fracture . Um, and just just for |
|
|
81:41 | one little thing here, I'll give an example. Say our source rocks |
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|
81:47 | , uh is more or less. , although it's got a lot of |
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|
81:52 | material, and it's got a lot carbonate in it, and so it's |
|
|
81:56 | be more brittle than a and, a classic derived, solicitous, rich |
|
|
82:07 | . So but a lot of the did early on in some of these |
|
|
82:13 | is if they had these areas where had a carbonate rich source rock, |
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|
82:21 | was brittle. One of the things they started looking for, uh, |
|
|
82:26 | their seismic is what areas had the flex oring going on. Other |
|
|
82:32 | Ah, if you have these flat sentimentally lime stones that air full of |
|
|
82:37 | material, all I have to do find a place where I can see |
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82:43 | flexing in the layer. Um and I know that that might be an |
|
|
82:51 | that has more fracturing than an area still flatlining. In other words, |
|
|
82:56 | been no, no structural Fletcher, I have a brittle rock and I |
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83:02 | this structural Fletcher, I'm gonna have have fracturing in there. And so |
|
|
83:06 | be natural fracturing that could be And there's there are places where |
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|
83:13 | we, uh, actually work in unconventional where we don't have to fracture |
|
|
83:18 | the fracturing there is already better. also, if you do go in |
|
|
83:22 | do fracturing Ah, you know, it zits more brittle, the less |
|
|
83:31 | it is. And the more carbonate that is, the more likely we |
|
|
83:35 | that units going toe fracture a little better. Another thing that you can |
|
|
83:40 | figure out from the stress fields that from some of that structural flexing and |
|
|
83:47 | structural activity like faulting and that sort thing. You can get a nice |
|
|
83:53 | with the primary fracture, directions might occurring in, uh And then, |
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|
84:00 | course, another thing you're gonna be to find out is where is the |
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|
84:05 | part of the oil source and so you start drilling. You have this |
|
|
84:13 | plan, what often happens? You may not know any of |
|
|
84:18 | Somebody's tapped into it. And just of the way the leases situated, |
|
|
84:26 | starts drilling all their wells big horizontal northwest instead of instead of Northeast, |
|
|
84:37 | might be the better fracture, direction that you want to cut |
|
|
84:42 | Uh, so they just start drilling the wrong direction. But once you've |
|
|
84:46 | that, because you're drilling all these and trying to monetize this thing really |
|
|
84:50 | and you want it to fit within leased lines. Ah, uh, |
|
|
84:56 | you've done that, you might realize you're not drilling in the right |
|
|
85:01 | Thio two more or less have a of times that it oftentimes it's not |
|
|
85:08 | but often times if you have your fractures perpendicular to the well bore when |
|
|
85:13 | dio you're fracturing, you're going toe that natural fracture. So that's many |
|
|
85:21 | the way you want to do Uh, unfortunately, a lot of |
|
|
85:25 | for speed, uh, people don't orient things in the right direction because |
|
|
85:32 | don't really have time to do But once you've drilled, uh, |
|
|
85:37 | 10 or 12 of these laterals, , you're gonna have an idea in |
|
|
85:43 | future, for in the future, direction has the best porosity and permeability |
|
|
85:48 | direction from that original? Well, getting richer oil sources and you might |
|
|
85:55 | able to see in one direction you're to richer oil. Uh, oil |
|
|
86:02 | . In other words, there's more . Mm uh huh. To the |
|
|
86:07 | of my field. And there is the north of the minefield. And |
|
|
86:10 | starts to help you get in idea what direction. You should be moving |
|
|
86:15 | . So you sort of, unlike is where we start from the outside |
|
|
86:20 | look for these things. With a you've drilled, you've drilled that initial |
|
|
86:26 | , and you're probably drilling a lot wells because you need to keep that |
|
|
86:29 | flow going. You know, you're it from that that bench, so |
|
|
86:34 | speak that you've that you've got your pipe into and you're trying to monetize |
|
|
86:41 | thing is, though, it is . But as you're drilling it from |
|
|
86:45 | inside out, you're finding out that not homogeneous, and you're finding out |
|
|
86:50 | there actually is variability. And now starting toe learn from the inside out |
|
|
86:55 | of from the outside in. I'm to learn where I should be putting |
|
|
87:01 | next drill, uh, lateral my next laterals, and where I |
|
|
87:07 | be buying extra acreage that I hadn't about in the past. Okay, |
|
|
87:14 | I think we're going to take a . It sounds like people might be |
|
|
87:18 | , but how long has this Yeah, eyes. It been an |
|
|
87:30 | yet, or an hour and a . But we started around. |
|
|
87:39 | It's been close to an hour and half right now. Okay, so |
|
|
87:44 | go ahead and take a 10 minute and I will try to pause the |
|
|
87:58 | if I can get out of |
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