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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
卷号	0期号:2页码:317-328
关键词	塔里木盆地北部 碳同位素示踪 中上奥陶统 古气候意义 早期 地层对比 牙形石动物群 海平面波动
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/4350984
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, Chengdu 610059, China 2.[2]Institute of Exploration and Development, Northwest OiIfield Company, SINOPEC, Urumqi 830011, China 3.[3]Institute of DeepSea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China
推荐引用方式 GB/T 7714	Cunge Liu,Guorong Li,Dawei Wang,等. Middle-Upper Ordovician （Darriwilian-Early Katian） Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China： Implications for Stratigraphic Correlation and Paleoclimate[J],2016,0(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.,0(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".0.2(2016):317-328.

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