The response of Os isotope in a ferromanganese crust from the West Pacific to paleaoceanographic events
Li, Jiangshan1,2; Ren, Xiangwen1,2; Shi, Xuefa1; Liu, Jihua1
2009
会议日期9 20, 2009 - 9 24, 2009
会议地点Chennai, India
页码37-41
英文摘要This paper researches the ferromanganese crust MHD79 from bottom to top 20 Os isotope data from the Central Pacific. The results showed that: in the Ferromanganese crust MHD79, each187Os/188Os value low point corresponds to the Os content high point, and corresponds to a large-scale volcanic (magmatic) activity or meteorite impact event. In the early three stages of the ferromanganese crust MHD79, Os content gradually increased with the decreasing of187Os/188Os, which demonstrates that Os content correlated with187Os/188Os negatively during this period; in the stages IV and V, the Os contents still correlated negatively with the187Os/188Os, but the 187Os/188Os value increased gradually; in the stage VI, the Os contents increased and correlated positively with the 1870s/1880s. The evolution of Os contents and187Os/ Os in the ferromanganese crust MHD79 suggested that, mantle and extraterrestrial material were the main contributors to the Os in the ocean relative to terrestrial material from late Cretaceous to Paleocene; Thereafter, the terrestrial material input increased gradually; after Oligocene, the terrestrial material input increased rapidly and became the main contributor for the Os in the ocean. Copyright © 2009 by The International Society of Offshore and Polar Engineers (ISOPE).
会议录Proceedings of the ISOPE Ocean Mining Symposium
会议录出版者International Society of Offshore and Polar Engineers
语种英语
内容类型会议论文
源URL[http://ir.fio.com.cn:8080/handle/2SI8HI0U/7126]  
专题业务部门_海洋地质与地球物理研究室
作者单位1.Key Laboratory of Marine Sedimentology and Environmental Geology of State Oceanic Administration, First Institute of Oceanography, State Oceanic Administration, Qingdao, China;
2.Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
推荐引用方式
GB/T 7714
Li, Jiangshan,Ren, Xiangwen,Shi, Xuefa,et al. The response of Os isotope in a ferromanganese crust from the West Pacific to paleaoceanographic events[C]. 见:. Chennai, India. 9 20, 2009 - 9 24, 2009.
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