I. Ya. Bogatyreva, Yu. A. Kotochkova, N. S. Balushkina, O. V. Khotylev, M. M. Fomina, N. A. Tyurina, B. I. Yablonovskiy, G. A. Kalmykov
{"title":"Structural-Facies Typification of Sections of the Bazhenov High-Carbon Formation of the West Siberian Basin","authors":"I. Ya. Bogatyreva, Yu. A. Kotochkova, N. S. Balushkina, O. V. Khotylev, M. M. Fomina, N. A. Tyurina, B. I. Yablonovskiy, G. A. Kalmykov","doi":"10.3103/s0145875224700261","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>The Bazhenov high-carbon formation is a set of marine pelitomorphic deposits enriched in organic matter, which accumulated under conditions of subsidence of the bottom of the sedimentary basin, which was not compensated by sediments. The formation contains hydrocarbons in its entire volume and is a promising source for expanding the hydrocarbon resource base. This article presents a set of the results of core studies and interpretation of well logging and seismic survey data for structural and facies typification of sections of the Bazhenov high-carbon formation throughout the area of its distribution. A multi-faceted approach to studying rocks has made it possible to divide the West Siberian basin into 13 structural-facies zones, each of which has its own structural features of the Bazhenov high-carbon formation section, including the total thickness, the presence of lithological and geophysical members and lithophysical types of rocks in the members, and the total concentration of organic carbon. In the future, this typification of sections will make it possible to simplify the modeling of the properties of Bazhenov high-carbon formation and the prediction of the most prospective areas.</p>","PeriodicalId":44391,"journal":{"name":"Moscow University Geology Bulletin","volume":null,"pages":null},"PeriodicalIF":0.3000,"publicationDate":"2024-07-17","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/s0145875224700261","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 Bazhenov high-carbon formation is a set of marine pelitomorphic deposits enriched in organic matter, which accumulated under conditions of subsidence of the bottom of the sedimentary basin, which was not compensated by sediments. The formation contains hydrocarbons in its entire volume and is a promising source for expanding the hydrocarbon resource base. This article presents a set of the results of core studies and interpretation of well logging and seismic survey data for structural and facies typification of sections of the Bazhenov high-carbon formation throughout the area of its distribution. A multi-faceted approach to studying rocks has made it possible to divide the West Siberian basin into 13 structural-facies zones, each of which has its own structural features of the Bazhenov high-carbon formation section, including the total thickness, the presence of lithological and geophysical members and lithophysical types of rocks in the members, and the total concentration of organic carbon. In the future, this typification of sections will make it possible to simplify the modeling of the properties of Bazhenov high-carbon formation and the prediction of the most prospective areas.
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.
求助内容：
应助结果提醒方式：
京公网安备 11010802042870号
