Organic Geochemistry of the Early Jurassic Oil Shale from the Shuanghu Area in Northern Tibet and the Early Toarcian Oceanic Anoxic Event

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Organic Geochemistry of the Early Jurassic Oil Shale from the Shuanghu Area in Northern Tibet and the Early Toarcian Oceanic Anoxic Event
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1 Introduction The concept of the Oceanic Anoxic Event (OAE) was introduced by Schlanger and Jenkyns (1976) to delineate a period of time characterized by abnormally high depositional and preservational rates of organic carbon in favorable marine environments in many parts of the globe. This concept, with particular respect to the Cretaceous, has since been discussed, elucidated, and refined by many researchers (e.g. Schlanger et al., 1987; Jenkyns, 1985). The signatures, causes and models…

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CHEN Lan, YI Haisheng, HU Ruizhong, ZHONG Hong, ZOU Yanrong Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou Graduate School of Chinese Academy of Sciences, Beijing Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong .2005. Organic Geochemistry of the Early Jurassic Oil Shale from the Shuanghu Area in Northern Tibet and the Early Toarcian Oceanic Anoxic Event[J]. Acta Geologica Sinica(),79(3):

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