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	Water redox conditions and environment for source rock deposition in lacustrine during the Initial Eocene Thermal Maximum(IETM):A case study on the Paleogene Kongdian Formation in the Dongying Sag
	Liu, Ping; Tan, Xianfeng; Chen, Qing; Wang, Jia; Liang, Mai; Wang, Ping; Wang, Weiqing
	2017
卷号	38页码:39-48
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/3408817
专题	成都理工大学
作者单位	1.[1] Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan, 610059, China 2.[2] Chongqing Key Laboratory of Complex Oil and Gas Exploration and Development, Chongqing, 401331, China 3.[3] Chongqing University of Science and Technology, Chongqing, 401331, China 4.[4] Geological Scientific Research Institute of Shengli Oilfield Company, SINOPEC, Dongying, Shandong, 257015, China
推荐引用方式 GB/T 7714	Liu, Ping,Tan, Xianfeng,Chen, Qing,et al. Water redox conditions and environment for source rock deposition in lacustrine during the Initial Eocene Thermal Maximum(IETM):A case study on the Paleogene Kongdian Formation in the Dongying Sag[J],2017,38:39-48.
APA	Liu, Ping.,Tan, Xianfeng.,Chen, Qing.,Wang, Jia.,Liang, Mai.,...&Wang, Weiqing.(2017).Water redox conditions and environment for source rock deposition in lacustrine during the Initial Eocene Thermal Maximum(IETM):A case study on the Paleogene Kongdian Formation in the Dongying Sag.,38,39-48.
MLA	Liu, Ping,et al."Water redox conditions and environment for source rock deposition in lacustrine during the Initial Eocene Thermal Maximum(IETM):A case study on the Paleogene Kongdian Formation in the Dongying Sag".38(2017):39-48.

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