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)
- Авторы: Hao Yuexiang 1, Shardanova T.A.1, Chongxing H.2
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Учреждения:
- Department of Geology, Moscow State University
- Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County
- Выпуск: Том 74, № 5 (2019)
- Страницы: 510-515
- Раздел: 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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Аннотация
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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Об авторах
Hao Yuexiang
Department of Geology, Moscow State University
Автор, ответственный за переписку.
Email: yuriiyx@hotmail.com
Россия, Moscow, 119991
T. Shardanova
Department of Geology, Moscow State University
Автор, ответственный за переписку.
Email: tshaedanova@mail.ru
Россия, Moscow, 119991
Huang Chongxing
Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County
Автор, ответственный за переписку.
Email: huangcx_dyy@cnpc.com.cn
Китай, Chengdu, Sichuan Province, 610051
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