中国科学院南海海洋研究所机构知识库
Advanced  
SCSIO OpenIR  > 中科院边缘海地质重点实验室  > 期刊论文
学科主题: Geosciences, Multidisciplinary; Oceanography
题名: Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation
作者: Liu, ZF ; Tuo, ST ; Colin, C ; Liu, JT ; Huang, CY ; Selvaraj, K ; Chen, CTA ; Zhao, YL ; Siringan, FP ; Boulay, S ; Chen, Z
通讯作者: lzhifei@mail.tongji.edu.cn
关键词: clay minerals ; surface sediments ; provenance ; South China Sea ; Taiwan
刊名: MARINE GEOLOGY
发表日期: 2008
卷: 255, 期:40606, 页:149-155
收录类别: sci
部门归属: [Liu, Zhifei; Tuo, Shouting; Zhao, Yulong; Boulay, Sebastien] Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China; [Colin, Christophe] Univ Paris 11, CNRS, UMR 8148, Lab IDES, F-91405 Orsay, France; [Liu, James T.; Selvaraj, Kandasamy; Chen, Chen-Tung Arthur] Natl Sun Yat Sen Univ, Inst Marine Geol & Chem, Kaohsiung 80424, Taiwan; [Huang, Chi-Yue] Natl Cheng Kung Univ, Dept Earth Sci, Tainan 70101, Taiwan; [Siringan, Fernando P.] Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines; [Chen, Zhong] Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China
项目归属: 海洋地质
摘要: Results of clay mineralogy in 140 samples collected in major rivers and lakes in southwestern Taiwan and on the seafloor off Taiwan in the northeastern South China Sea (SCS), combined with clay mineral records of the Pearl River drainage basin, rivers in Luzon, and the South China shelf and slope, are used to semi-quantitatively evaluate the detrital fine-grained sediment contribution of Taiwan to the northern SCS. The clay mineral assemblage of the Taiwan-sourced sediments consists dominantly of illite (average 56%) and chlorite (41%), with very scarce kaolinite and smectite. Their respective distribution from the rivers and lakes to the seafloor off Taiwan does not show obvious basin-wide differences. Linear correlations of illite chemistry index with illite crystallinity and of illite crystallinity with kaolinite (%) present two end-members of provenances, the Pearl River and Taiwan, for the South China shelf and slope. Assuming that kaolinite in the northern SCS is provided completely from the Pearl River, the contribution of Taiwan in clay minerals is evaluated as 29% to the South China shelf and 23% to the South China slope, respectively. Accordingly, the contribution of the Pearl River to the South China shelf and slope is 52% and 31 %, respectively. The Luzon Arc accounts for the rest of clay mineral components for the northern SCS mainly by providing smectite. The Bashi Strait-crossed branches of the southward deep North Pacific Deep Water and the northward Surface Kuroshio Current in the western Pacific may transport Taiwan-sourced Suspended sediments westwards to the northern SCS. (C) 2008 Elsevier B.V. All rights reserved.
原文出处: 查看原文
WOS记录号: WOS:000261702800004
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/4520
Appears in Collections:中科院边缘海地质重点实验室_期刊论文

Files in This Item: Download All
File Name/ File Size Content Type Version Access License
Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation .pdf(2024KB)----开放获取--View Download

Recommended Citation:
Liu, ZF; Tuo, ST; Colin, C; Liu, JT; Huang, CY; Selvaraj, K; Chen, CTA; Zhao, YL; Siringan, FP; Boulay, S; Chen, Z.Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation,MARINE GEOLOGY,2008,255(40606):149-155
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Liu, ZF]'s Articles
[Tuo, ST]'s Articles
[Colin, C]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Liu, ZF]‘s Articles
[Tuo, ST]‘s Articles
[Colin, C]‘s Articles
Related Copyright Policies
Null
Social Bookmarking
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit
文件名: Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation .pdf
格式: Adobe PDF
所有评论 (0)
暂无评论
 
评注功能仅针对注册用户开放,请您登录
您对该条目有什么异议,请填写以下表单,管理员会尽快联系您。
内 容:
Email:  *
单位:
验证码:   刷新
您在IR的使用过程中有什么好的想法或者建议可以反馈给我们。
标 题:
 *
内 容:
Email:  *
验证码:   刷新

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.

 

 

Valid XHTML 1.0!
Copyright © 2007-2017  中国科学院南海海洋研究所 - Feedback
Powered by CSpace