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
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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 |
DOI | 10.1007/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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