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	Trace and rare earth element (REE) characteristics of mudstones from Eocene Pinghu Formation and Oligocene Huagang Formation in Xihu Sag, East China Sea Basin: Implications for provenance, depositional conditions and paleoclimate
	Xie, Guoliang; Shen, Yulin; Liu, Shugen; Hao, Weiduo
	2018
卷号	92页码:20-36
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/3404410
专题	成都理工大学
作者单位	1.[1]Chengdu Univ Technol, Coll Energy Resources, Chengdu 610059, Sichuan, Peoples R China 2.[2]Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China 3.[3]China Univ Min & Technol, Sch Resources & Geosci, Xuzhou 221008, Jiangsu, Peoples R China 4.[4]Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2R3, Canada
推荐引用方式 GB/T 7714	Xie, Guoliang,Shen, Yulin,Liu, Shugen,et al. Trace and rare earth element (REE) characteristics of mudstones from Eocene Pinghu Formation and Oligocene Huagang Formation in Xihu Sag, East China Sea Basin: Implications for provenance, depositional conditions and paleoclimate[J],2018,92:20-36.
APA	Xie, Guoliang,Shen, Yulin,Liu, Shugen,&Hao, Weiduo.(2018).Trace and rare earth element (REE) characteristics of mudstones from Eocene Pinghu Formation and Oligocene Huagang Formation in Xihu Sag, East China Sea Basin: Implications for provenance, depositional conditions and paleoclimate.,92,20-36.
MLA	Xie, Guoliang,et al."Trace and rare earth element (REE) characteristics of mudstones from Eocene Pinghu Formation and Oligocene Huagang Formation in Xihu Sag, East China Sea Basin: Implications for provenance, depositional conditions and paleoclimate".92(2018):20-36.

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