Email this article 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)
- Authors: Hao Yuexiang 1, Shardanova T.A.1, Chongxing H.2
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Affiliations:
- Department of Geology, Moscow State University
- Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County
- Issue: Vol 74, No 5 (2019)
- Pages: 510-515
- Section: Short Communications
- URL: https://journals.rcsi.science/0145-8752/article/view/175076
- DOI: https://doi.org/10.3103/S0145875219050156
- ID: 175076
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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.
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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
