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	Middle–Upper Ordovician(Darriwilian–Early Katian) Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China: Implications for Stratigraphic Correlation and Paleoclimate
	Cunge Liu; Guorong Li; Dawei Wang; Yongli Liu; Mingxia Luo; Xiaoming Shao
	2016
期号	2页码:317-328
URL标识	查看原文
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/4368817
专题	成都理工大学
作者单位	1.[1]State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology 2.[2]Institute of Exploration and Development,Northwest Oilfield Company, SINOPEC 3.[3]Institute of DeepSea Science and Engineering, Chinese Academy of Sciences
推荐引用方式 GB/T 7714	Cunge Liu,Guorong Li,Dawei Wang,et al. Middle–Upper Ordovician(Darriwilian–Early Katian) Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China: Implications for Stratigraphic Correlation and Paleoclimate[J],2016(2):317-328.
APA	Cunge Liu,Guorong Li,Dawei Wang,Yongli Liu,Mingxia Luo,&Xiaoming Shao.(2016).Middle–Upper Ordovician(Darriwilian–Early Katian) Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China: Implications for Stratigraphic Correlation and Paleoclimate.(2),317-328.
MLA	Cunge Liu,et al."Middle–Upper Ordovician(Darriwilian–Early Katian) Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China: Implications for Stratigraphic Correlation and Paleoclimate"..2(2016):317-328.

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