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)
- Авторлар: Hao Yuexiang 1, Shardanova T.A.1, Chongxing H.2
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Мекемелер:
- Department of Geology, Moscow State University
- Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County
- Шығарылым: Том 74, № 5 (2019)
- Беттер: 510-515
- Бөлім: Short Communications
- URL: https://journals.rcsi.science/0145-8752/article/view/175076
- DOI: https://doi.org/10.3103/S0145875219050156
- ID: 175076
Дәйексөз келтіру
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.
Негізгі сөздер
Авторлар туралы
Hao Yuexiang
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: yuriiyx@hotmail.com
Ресей, Moscow, 119991
T. Shardanova
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: tshaedanova@mail.ru
Ресей, Moscow, 119991
Huang Chongxing
Chuanging Drilling and Exploration Corporation Co., Ltd., Chenghua County
Хат алмасуға жауапты Автор.
Email: huangcx_dyy@cnpc.com.cn
ҚХР, Chengdu, Sichuan Province, 610051
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