Tectonic and eustatic control on the distribution of black-shale source beds in the Wufeng and Longmaxi formations (Ordovician-Silurian), South China

Author:

Su Wenbo,Li Zhiming,Ettensohn F. R.,Johnson M. E.,Huff W. D.,Wang Wei,Ma Chao,Li Lu,Zhang Lei,Zhao Huijing

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference74 articles.

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2. Chen H D, Ni X F, Tian J C, et al (2006a). Sequence stratigraphic framework of marine lower assemblage in South China and petroleum exploration. Oil and Gas Geology, 27(3): 370–377 (in Chinese with English abstract)

3. Chen J Q, Li Z M, Gong S Y, et al (1997). Lower and Middle Silurian sequence stratigraphy of northeastern Guizhou, China. Earth Sciences—Journal of China University of Geosciences, 22(6): 559–564 (in Chinese with English abstract)

4. Chen X, Rong J Y, Li Y, et al (2004). Facies patterns and geography of the Yangtze region, South China, through the Ordovician and Silurian transition. Palaeogeography, Palaeoclimatology, Palaeoecology, 204: 353–372

5. Chen X, Qiu J Y (1986). Ordovician palaeoenvironment reconstruction of Yichang area, Western Hubei. Journal of Stratigraphy, 10(1): 1–15 (in Chinese with English abstract)

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