Clay mineral distributions in the southern Yellow Sea and their significance

doi:10.1360/01we0011

IOCAS-IR > 海洋地质与环境重点实验室

	Clay mineral distributions in the southern Yellow Sea and their significance
	Wei, JW ; Shi, XF ; Li, GB ; Liang, RC
	2003-06-01
发表期刊	CHINESE SCIENCE BULLETIN
ISSN	1001-6538
卷号	48 页码:7-11
文章类型	Article
摘要	To better understand the characteristics of the clay minerals in the southern Yellow Sea, the X-ray quantitative determinations have been carried out for the surface samples obtained from the Yellow Sea. With newly compiled clay mineral synoptic maps, the depositional processes were described for four main clay minerals (illite, chlorite, kaolinite and smectite). The analysis shows that most clay minerals are of terrigenous source with the Huanghe River acting as the major sediment supplier. Besides, the source of muddy sediments in the Yellow Sea was also discussed. As for the central Yellow Sea mud (CYSM), the sediments in its northern part mainly come from the Huanghe River, and those in the rest are of multi-origin. Very similarly, a large amount of sediments in the northern part of the southeastern Yellow Sea Mud (SEYSM) derive from the Keum River and Yeong-san River, while those in the southern part are of multi-origin.; To better understand the characteristics of the clay minerals in the southern Yellow Sea, the X-ray quantitative determinations have been carried out for the surface samples obtained from the Yellow Sea. With newly compiled clay mineral synoptic maps, the depositional processes were described for four main clay minerals (illite, chlorite, kaolinite and smectite). The analysis shows that most clay minerals are of terrigenous source with the Huanghe River acting as the major sediment supplier. Besides, the source of muddy sediments in the Yellow Sea was also discussed. As for the central Yellow Sea mud (CYSM), the sediments in its northern part mainly come from the Huanghe River, and those in the rest are of multi-origin. Very similarly, a large amount of sediments in the northern part of the southeastern Yellow Sea Mud (SEYSM) derive from the Keum River and Yeong-san River, while those in the southern part are of multi-origin.
关键词	Clay Mineral Southern Yellow Sea Origin Muddy Sediments
学科领域	Multidisciplinary Sciences
DOI	10.1360/01we0011
收录类别	SCI
语种	英语
WOS记录号	WOS:000183335900002
引用统计	被引频次：18[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/3792
专题	海洋地质与环境重点实验室
作者单位	1.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao, Peoples R China 2.Acad Sinica, Inst Oceanol, Qingdao 266071, Peoples R China 3.Acad Sinica, Grad Sch, Beijing 100039, Peoples R China
推荐引用方式 GB/T 7714	Wei, JW,Shi, XF,Li, GB,et al. Clay mineral distributions in the southern Yellow Sea and their significance[J]. CHINESE SCIENCE BULLETIN,2003,48:7-11.
APA	Wei, JW,Shi, XF,Li, GB,&Liang, RC.(2003).Clay mineral distributions in the southern Yellow Sea and their significance.CHINESE SCIENCE BULLETIN,48,7-11.
MLA	Wei, JW,et al."Clay mineral distributions in the southern Yellow Sea and their significance".CHINESE SCIENCE BULLETIN 48(2003):7-11.

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