A Сomparative Analysis of Oils from Carbonate Sediments of the Upper Usolskaya Subformation and the Vendian–Cambrian Pay Horizons in the Central Part of the Nepsko-Botuobinskaya Anteclise

IF 0.3 Q4 GEOLOGY
I. V. Egorov, M. A. Bolshakova, O. V. Krylov
{"title":"A Сomparative Analysis of Oils from Carbonate Sediments of the Upper Usolskaya Subformation and the Vendian–Cambrian Pay Horizons in the Central Part of the Nepsko-Botuobinskaya Anteclise","authors":"I. V. Egorov, M. A. Bolshakova, O. V. Krylov","doi":"10.3103/s0145875223060066","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>The study of the prospects in the central part of the Nepsko-Botuobinskaya Anteclise is focused on the subsalt oil and gas bearing horizons of Group B (Osinsky, Upper Ust-Kutsky, Lower Ust-Kutsky, and Preobrazhensky) and Group V (terrigenous formations of Vendian age). However, higher, in the Lower–Middle Cambrian carbonate-halogen deposits, there are also promising horizons of Group A (Kelorsky, Atovsky, Khristoforovsky, and Balykhtinsky) whose sufficient oil and gas content was confirmed in the neighboring Angara-Lena stage and in the north of the Nepsko-Botuobinskaya Anteclise and its adjacent structures. This paper examines the results of geochemistry tests of oil samples from the Osinsky horizon (layer B1) and the nameless dolomite layer located between the salts in the lower part of the Upper Usolskaya Subformation, which was previously considered gas-bearing at best. The tests conducted by the method of chromatography-mass spectrometry and the comparison of geochemical parameters of oils from different reservoirs show the similarity of hydrocarbon fluids of the Upper Usolskaya Subformation and of underlying pay horizons, which makes it possible to attribute them to a single oil and gas bearing system.</p>","PeriodicalId":44391,"journal":{"name":"Moscow University Geology Bulletin","volume":null,"pages":null},"PeriodicalIF":0.3000,"publicationDate":"2024-02-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Moscow University Geology Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3103/s0145875223060066","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

The study of the prospects in the central part of the Nepsko-Botuobinskaya Anteclise is focused on the subsalt oil and gas bearing horizons of Group B (Osinsky, Upper Ust-Kutsky, Lower Ust-Kutsky, and Preobrazhensky) and Group V (terrigenous formations of Vendian age). However, higher, in the Lower–Middle Cambrian carbonate-halogen deposits, there are also promising horizons of Group A (Kelorsky, Atovsky, Khristoforovsky, and Balykhtinsky) whose sufficient oil and gas content was confirmed in the neighboring Angara-Lena stage and in the north of the Nepsko-Botuobinskaya Anteclise and its adjacent structures. This paper examines the results of geochemistry tests of oil samples from the Osinsky horizon (layer B1) and the nameless dolomite layer located between the salts in the lower part of the Upper Usolskaya Subformation, which was previously considered gas-bearing at best. The tests conducted by the method of chromatography-mass spectrometry and the comparison of geochemical parameters of oils from different reservoirs show the similarity of hydrocarbon fluids of the Upper Usolskaya Subformation and of underlying pay horizons, which makes it possible to attribute them to a single oil and gas bearing system.

Abstract Image

上乌索尔斯卡亚亚层碳酸盐沉积物和尼泊尔-博图宾斯卡亚反地层中部文迪-寒武纪海平面的油类对比分析
摘要 对 Nepsko-Botuobinskaya Anteclise 中部地区前景的研究主要集中在 B 组(Osinsky、Upper Ust-Kutsky、Lower Ust-Kutsky 和 Preobrazhensky)和 V 组(Vendian 时代的陆相地层)的盐下含油和含气地层。然而,在更高的下-中寒武统碳酸盐-卤化物矿床中,也有前景看好的 A 组地层(Kelorsky、Atovsky、Khristoforovsky 和 Balykhtinsky),其充足的石油和天然气含量已在邻近的安加拉-勒拿河期和 Nepsko-Botuobinskaya Anteclise 北部及其邻近构造中得到证实。本文研究了对来自奥辛斯基地层(B1层)和位于上乌索尔斯卡亚岩层下部盐类之间的无名白云岩层的石油样本进行地球化学测试的结果。用色谱-质谱法进行的测试以及对不同储油层的石油地质化学参数进行的比较表明,上乌索列斯卡亚岩层和下层地层的碳氢化合物流体具有相似性,因此可以将它们归属于一个单一的含油气系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
文献相关原料
公司名称 产品信息 采购帮参考价格
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信