Features of the Structure of Carbon-Rich Rocks (Based on the Example of the Lower Silurian Sediments of the Sichuan Depression of the Yangtze Platform)


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Abstract

The petrophysical, geochemical, and lithological features of the structure of graptolite shales from the lower part of the Longmaxi Formation of the Lower Silurian age of the Sichuan Province of the People’s Republic of China are considered. The basic patterns of the formation of carbon-rich sediments in the intrashelf depressions are revealed.

About the authors

Hao Yuexiang

Department of Geology, Moscow State University

Author for correspondence.
Email: yuriiyx@hotmail.com
Russian Federation, Moscow, 119991

T. A. Shardanova

Department of Geology, Moscow State University

Author for correspondence.
Email: tshaedanova@mail.ru
Russian Federation, Moscow, 119991

Huang Chongxing

Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County

Author for correspondence.
Email: huangcx_dyy@cnpc.com.cn
China, Chengdu, Sichuan Province, 610051

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