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	Provenance Study of Fe-Ti Oxide Minerals in the Quaternary Sediments in Yichang Area and Its Implication of Formation Time of the Yangtze Three Gorges, China
	XIANG Fang; DU Wen; HUANG Henxu; KANG Dongya; ZHU Hongbo; FENG Qin
	2018
卷号	92期号:4页码:1598-1608
关键词	形成时间 氧化物 矿物质 三峡 沉积 四级 起源 学习
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/4679475
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]Shangdong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shangdong University of Science and Technology, Qingdao 266590, China 3.[3]Institute of sedimentary geology, Chengdu University of Technology, Chengdu 610059, China
推荐引用方式 GB/T 7714	XIANG Fang,DU Wen,HUANG Henxu,et al. Provenance Study of Fe-Ti Oxide Minerals in the Quaternary Sediments in Yichang Area and Its Implication of Formation Time of the Yangtze Three Gorges, China[J],2018,92(4):1598-1608.
APA	XIANG Fang,DU Wen,HUANG Henxu,KANG Dongya,ZHU Hongbo,&FENG Qin.(2018).Provenance Study of Fe-Ti Oxide Minerals in the Quaternary Sediments in Yichang Area and Its Implication of Formation Time of the Yangtze Three Gorges, China.,92(4),1598-1608.
MLA	XIANG Fang,et al."Provenance Study of Fe-Ti Oxide Minerals in the Quaternary Sediments in Yichang Area and Its Implication of Formation Time of the Yangtze Three Gorges, China".92.4(2018):1598-1608.

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