Depositional architecture of the late Ordovician drowned carbonate platform margin and its responses to sea-level fluctuation in the northern slope of the Tazhong region, Tarim Basin-Reference-Cited by-同舟云学术

Depositional architecture of the late Ordovician drowned carbonate platform margin and its responses to sea-level fluctuation in the northern slope of the Tazhong region, Tarim Basin

Published:2010-08-03 Issue:3 Volume:7 Page:323-336
ISSN:1672-5107
Container-title:Petroleum Science
language:en
Short-container-title:Pet. Sci.

Author:

Yang Xiaofa,Lin Changsong,Yang Haijun,Han Jianfa,Liu Jingyan,Zhang Yanmei,Peng Li,Jing Bing,Tong Jianyu,Wang Haiping,Li Huanpu

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology,Geophysics,Energy Engineering and Power Technology,Geotechnical Engineering and Engineering Geology,Fuel Technology

Link

http://link.springer.com/content/pdf/10.1007/s12182-010-0074-0.pdf

Reference37 articles.

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3. Chen X J, Cai X Y, Xu X H, et al. The research on sedimentation features in Cambrian-Ordovician sequence frame in the center of the Tarim Basin. Xinjiang Geology. 2006. 24(3): 276–280 (in Chinese)

4. Chen X, Zhao Z J, Zhang B M, et al. Sedimentary model to Lianglitage Formation of Upper Ordovician in the northern margin of isolated platform in the center of the Tarim Basin. Acta Sedimentologica Sinica. 2009. 27(5): 1002–1011 (in Chinese)

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