中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Os isotope dating and growth hiatuses of Co-rich crust from central Pacific

文献类型:期刊论文

作者Li JiangShan1,2,3; Fang NianQiao1; Qu WenJun4; Ding Xuan1; Gao LianFeng5; Wu ChangHang1; Zhang Zhenguo5
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2008-10-01
卷号51期号:10页码:1452-1459
关键词Central Pacific Co-rich Crust Os Isotope Dating Growth Hiatus
ISSN号1006-9313
DOI10.1007/s11430-008-0100-x
文献子类Article
英文摘要Up to now, accurate determination of the growth age and hiatuses of the Co-rich crust is still a difficult work, which constrains the researches on the genesis, growth process, controlling factors, regional tectonics, paleo-oceanographic background, etc. of the Co-rich crust. This paper describes our work in determining the initial growth age of the Co-rich crust to be of the late Cretaceous Campanian Stage (about 75-80 Ma), by selecting the Co-rich crust with clear multi-layer structures in a central Pacific seamount for layer-by-layer sample analysis and using a number of chronological methods, such as Co flux dating, dating by correlation with Os-187/Os-188 evolution curves of seawater, and stratigraphic division by calcareous nannofossils. We have also discovered growth hiatuses with different time intervals in the early Paleocene, middle Eocene, late Eocene and early-middle Miocene, respectively. These results have provided an important age background for further researches on the Co-rich crust growth process and the paleo-oceanographic environment evolution thereby revealed in the said region.; Up to now, accurate determination of the growth age and hiatuses of the Co-rich crust is still a difficult work, which constrains the researches on the genesis, growth process, controlling factors, regional tectonics, paleo-oceanographic background, etc. of the Co-rich crust. This paper describes our work in determining the initial growth age of the Co-rich crust to be of the late Cretaceous Campanian Stage (about 75-80 Ma), by selecting the Co-rich crust with clear multi-layer structures in a central Pacific seamount for layer-by-layer sample analysis and using a number of chronological methods, such as Co flux dating, dating by correlation with Os-187/Os-188 evolution curves of seawater, and stratigraphic division by calcareous nannofossils. We have also discovered growth hiatuses with different time intervals in the early Paleocene, middle Eocene, late Eocene and early-middle Miocene, respectively. These results have provided an important age background for further researches on the Co-rich crust growth process and the paleo-oceanographic environment evolution thereby revealed in the said region.
学科主题Geosciences, Multidisciplinary
URL标识查看原文
语种英语
WOS记录号WOS:000259790100009
公开日期2010-12-24
源URL[http://ir.qdio.ac.cn/handle/337002/5041]  
专题海洋研究所_海洋地质与环境重点实验室
作者单位1.China Univ Geosci, Sch Marine, Beijing 100083, Peoples R China
2.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China
3.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
4.Natl Res Ctr Geoanal, Beijing 100037, Peoples R China
5.Hebei Polytech Univ, Tangshan 063009, Peoples R China
推荐引用方式
GB/T 7714
Li JiangShan,Fang NianQiao,Qu WenJun,et al. Os isotope dating and growth hiatuses of Co-rich crust from central Pacific[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2008,51(10):1452-1459.
APA Li JiangShan.,Fang NianQiao.,Qu WenJun.,Ding Xuan.,Gao LianFeng.,...&Zhang Zhenguo.(2008).Os isotope dating and growth hiatuses of Co-rich crust from central Pacific.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,51(10),1452-1459.
MLA Li JiangShan,et al."Os isotope dating and growth hiatuses of Co-rich crust from central Pacific".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 51.10(2008):1452-1459.

入库方式: OAI收割

来源:海洋研究所

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