Sedimentary facies and material source of core DGKS9617 in the East China Sea

	Sedimentary facies and material source of core DGKS9617 in the East China Sea
	Yu, H ; Li, ZX ; Xiong, YQ ; Saito, Y ; Wang, KS ; Chung, KH ; Shin, YH ; Park, SN ; Cho, HS ; Yoo, SA
	2005
关键词	East China Sea material source heavy mineral elementary geochemistry
卷号	277-279
页码	410-417
英文摘要	A piston core DGKS9617, recovered from the northern part of the inner shelf of the East China Sea (ECS) is divided into two sedimentary facies: a tidal shallow marine facies (55-850 cm) and a shallow marine facies (0-55 cm). Although the sedimentary environments of its upper and lower parts are different, the provenance of the whole core does not change. The heavy mineral assemblage, the results of the discrimination function of Fe, Mn, V, Cr, Ni, Cu and Zn, the carbonate content and the Ba-Sr-Zn ternary diagram consistently show that the heavy mineral and geochemical characteristics of core DGKS9617 are similar to that of the Yangtze River sediments and that its sediment is mainly provided by the Yangtze River.
会议录	ON THE CONVERGENCE OF BIO-INFORMATION-, ENVIRONMENTAL-, ENERGY-, SPACE- AND NANO-TECHNOLOGIES, PTS 1 AND 2
会议录出版者	TRANS TECH PUBLICATIONS LTD
会议录出版地	BRANDRAIN 6, CH-8707 ZURICH-UETIKON, SWITZERLAND
语种	英语
WOS研究方向	Engineering ; Materials Science
WOS记录号	WOS:000227164500068
内容类型	会议论文
源URL	[http://ir.fio.com.cn/handle/2SI8HI0U/5301]
专题	自然资源部第一海洋研究所
作者单位	1.Ocean Univ China, Qingdao, Peoples R China; 2.State Ocean Adm, Inst Oceanog 1, Qingdao, Peoples R China; 3.AIST, Geol Survey Japan, MRE, Tsukuba, Ibaraki 3058567, Japan
推荐引用方式 GB/T 7714	Yu, H,Li, ZX,Xiong, YQ,et al. Sedimentary facies and material source of core DGKS9617 in the East China Sea[C]. 见:.