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00:10 | testing testing. Okay. All So, um, any other questions |
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00:16 | the strata graphic cross sections? Uh huh. That's right Between the two |
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00:34 | fields. Yeah. Yeah. All right. You guys one. |
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00:48 | let's finish up our discussion with if want to talk about the final exam |
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00:53 | you've got some more questions. D. All right. So the |
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01:04 | is Wednesday. It's here in Yeah. Three hours shouldn't take three |
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01:12 | , but you have three hours, you certainly have more time to go |
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01:17 | and double check. Triple check. . Have time for that. Compared |
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01:20 | the one our exams we had for 50% of your grades. So, |
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01:25 | know anything I covered in the first exams. This fair game. All |
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01:31 | . And I think you should make anything you missed in the first two |
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01:37 | is you better know that material. right. I mean, I can't |
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01:42 | ask every question that you missed, you can count on me asking something |
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01:47 | that I saw a lot of you the first two exams. I'm going |
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01:50 | ask again. I probably rephrase All right. So it's not just |
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01:55 | repetition of what I gave you but yeah. Um uh I |
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02:15 | I can read through this, but mean, you can read this as |
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02:18 | as I can. But I what are the highlights of this |
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02:25 | I mean the highlights of the segment I didn't have a lot of time |
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02:29 | talk about the details of the components make up typical shell and deep marine |
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02:32 | . So I'm not going to test on on that kind of detail because |
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02:36 | didn't spend much time talking about But we talked about, you |
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02:41 | the classical environments of shallow d. deposition right from the modern and all |
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02:46 | variations on the theme depending on where at paleo geographically. You need to |
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02:52 | those relationships, right? You need understand the basis for the member models |
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02:57 | talked about All right. I I've already tested you on some of |
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03:00 | , but you know, that would back into play. You need to |
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03:05 | the diabetic aspects of the carbonates. talked about both limestone, die genesis |
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03:10 | dehumanization. Ah different pathways for creating and permeability. The tiny relationships. |
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03:20 | ? Early processes versus later processes. I think I think we've had this |
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03:34 | about geometry enough that you have, hope you feel have a feel for |
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03:37 | now. Right. So, um , certainly need to all the stuff |
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03:52 | had this discussion about with the simple contact concept of winning and Stokes is |
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03:59 | . Whether it's applied to just the record in general and trying to see |
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04:04 | carbonates are put together or whether it's to reservoir zoning. You need to |
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04:10 | need to understand that there will be questions about that. Getting into that |
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04:14 | of the aspect again. And and there'll be a lot of questions about |
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04:23 | different play types. I mean the point of this discussion is to get |
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04:28 | up to speed on carbonate plays, ? I mean this is a master's |
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04:31 | in petroleum geology. Right? So supposed to look, you're supposed to |
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04:35 | something about the the different reservoir aspects with these carbonates, right? And |
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04:42 | context I used was the play right? Interplay between reservoir source and |
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04:49 | and then the trapping mechanism. And we spent a lot of time relating |
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04:53 | back to the general setting on a scale and then on a local |
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04:58 | And we talked about the geometry. of these play types evolved through |
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05:03 | So there'll be questions about that and probably probably ask you for maybe bringing |
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05:09 | an analog. Right? So be with some of the analog we talked |
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05:14 | , not the ones that I showed couple of slides on, but the |
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05:18 | that I really went into detail about , you should have some feel for |
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05:22 | nature of that, how that plays together and um and what was the |
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05:27 | control or what was the digest I might give you an option of |
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05:33 | one play and then talking about one way to either preserved ferocity or or |
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05:40 | . So. Mhm. Yeah. . And I've talked a lot about |
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05:55 | role of structuring. So what you , you'll be tested on some aspects |
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05:58 | that, right? Either how it topography or how sets up entrapment of |
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06:05 | or how it sets up favorable die . So again, be familiar with |
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06:11 | of that and some of the case we talked about that might relate back |
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06:15 | that. I might ask you to on a case study. Okay, |
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06:19 | that into the discussion. Things like . So All right. So, |
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06:26 | don't know how many questions I'm gonna yet, but uh I just started |
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06:33 | on it. So we'll see everybody questions or comments. Right, expect |
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06:47 | huh, specific. Uh huh. huh. I don't know. I |
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06:58 | think I'll ask specific examples. I you to understand the play concept more |
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07:05 | than an individual field. But I ask you uh for a couple of |
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07:10 | points. Can you bring in an for that plate type or something like |
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07:14 | ? So and maybe talk a little more about I might ask you a |
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07:18 | questions about that analog if you if can do it. Right? So |
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07:24 | is sort of what separates everybody. ? How how well they understand the |
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07:28 | and how familiar they are with some the analog. So again, things |
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07:35 | I skipped over. There was some that I skipped over a little bit |
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07:38 | quickly in terms of examples are not to ask anything about those, but |
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07:43 | each of the major play types. think I took you through at least |
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07:46 | or two different areas, right? one or two different analog really went |
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07:52 | detail about how the geology proved up of the controls on the show why |
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07:59 | play exists where it exists. Remember some of the platform mountain |
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08:04 | Why do they exist really exist because paleo topography, whatever that is. |
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08:08 | the assault related or inherited topography from cycle or structural topography and then the |
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08:17 | force to drive that deposition. Platform margin stuff is driven by oceanic |
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08:24 | . But things that occur way back board that have research grain stones like |
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08:29 | talked about that's driven by trade Right. So stuff like that. |
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08:43 | think you guys will do just Take your time. The thing Now |
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08:48 | sort of know how I've I'm not not going to change the style of |
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08:52 | . It's not going to be much from what you've had for the first |
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08:55 | . Doing okay. It's just a opportunity for you to to to bump |
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09:00 | your grade quite a bit. All right. Anything else? |
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09:25 | Yes. It's not that it's Is that Yeah, I mean we |
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09:34 | we showed a lot of different pathways process the evolution. Right. I |
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09:39 | , some some some of the reservoirs really well because they were demonetized. |
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09:45 | ? Some did really well because you ferocity. So the question is how |
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09:49 | you preserve that ferocity? And then did well because you created porosity either |
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09:55 | and you held onto it or Yeah. Right, because the burial |
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10:00 | or something like that. So So I might I might ask you |
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10:06 | questions like here, here, here's pathway, another process evolution. What |
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10:10 | it imply about where the fluids coming or what the fluid chemistry was or |
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10:15 | like that? Okay. Mhm. that would get back to some of |
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10:19 | discussion we had about die genesis. controls the different pathways for making secondary |
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10:26 | lime stones or and Dolomites to We showed I showed you two ways |
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10:31 | make secondary pressing dollar stone. One just to take the limestone and progressively |
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10:36 | ties it to that point where the grains dissolved out. But I also |
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10:42 | you through a couple of case the keg river and the Ellenberger where |
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10:46 | process there because you don't notice first then he brought another fluid through to |
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10:51 | out and create that final secondary So, okay. All right, |
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11:05 | luck. See you Wednesday 6:00, , 6-9 here and Utah is going |
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11:14 | open the door for us. So . All right, we'll see you |
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