中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sedimentary response to volcanic activity in the Okinawa Trough since the last deglaciation

文献类型:CNKI期刊论文

作者Jiang FQ(蒋富清); Li AC(李安春); Li TG(李铁刚)
发表日期2010-02-15
出处Chinese Journal of Oceanology and Limnology
关键词sediment ash layer last deglaciation Okinawa Trough
英文摘要To investigate the relationship between volcanic activity and sediment record on regional and temporal scales,158 surface sediment samples were collected from the East China Sea Shelf to the northern Okinawa Trough (OT),and two cores recovered in the northern and southern OT,respectively.Mineralogy,grain-size,and geochemical analyses of those samples show that:1) volcanic glass,volcanic-type pyroxene,hypersthenes,and magnetite increase in sediment influenced by volcanic activity;2) sediment grain sizes (and also silt content) increase in ash layers;and 3) the contents of Na2O and Zr are higher,while terrigenous elements,e.g.,TFe2O3 and K2O,and biogenous compositions,e.g.,CaO and Sr,are relatively lower in ash layers than those of non-ash layers.The distribution of volcanic ash has three distinguishing characteristics:1) volcanic ash is more abundant in the northern and central OT than the southern OT;2) volcanic ash increases from continental shelf to the trough;3) the sediment during the last 12 000 a suggests stronger volcanic events than during 15 000-12 000 a.The eruptive locations,frequency,and volume of calderas are among the most important factors controlling the distributions of volcanic ash.In addition,the main Kuroshio warm current that extends northward probably impeded the diffusion of volcanic ash to the west and south in the OT.However,a southward current probably carried some volcanic ash toward southern OT.
文献子类CNKI期刊论文
资助机构Supported by the Pilot Project of the National Knowledge Innovation Program of the Chinese Academy of Science (No. KZCX2-YW-221) ; the National Natural Science Foundation of China (No. 40506016,90411014 and 40976026) ; National Basic Research Program of China (No. 2007CB815903)
v.28期:01页:173-184
语种英文;
分类号P317
ISSN号0254-4059
源URL[http://ir.qdio.ac.cn/handle/337002/192249]  
专题中国科学院海洋研究所
作者单位KeyLaboratoryofMarineGeologyandEnvironment,InstituteofOceanology,ChineseAcademyofSciences
推荐引用方式
GB/T 7714
Jiang FQ,Li AC,Li TG. Sedimentary response to volcanic activity in the Okinawa Trough since the last deglaciation. 2010.

入库方式: OAI收割

来源:海洋研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。