洋中脊热液系统中的锇及其同位素

黄威; 陶春辉; 李军; 孙治雷; 邓希光; 崔汝勇

doi:10.3799/dqkx.2016.036

Volume 41 Issue 3

Mar. 2016

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Huang Wei, Tao Chunhui, Li jun, Sun Zhilei, Deng Xiguang, Cui Ruyong, 2016. Osmium Isotopic Compositions and Osmium Distribution in the Mid-Ocean Ridge Hydrothermal System. Earth Science, 41(3): 441-451. doi: 10.3799/dqkx.2016.036

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Huang Wei, Tao Chunhui, Li jun, Sun Zhilei, Deng Xiguang, Cui Ruyong, 2016. Osmium Isotopic Compositions and Osmium Distribution in the Mid-Ocean Ridge Hydrothermal System. Earth Science, 41(3): 441-451. doi: 10.3799/dqkx.2016.036

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Osmium Isotopic Compositions and Osmium Distribution in the Mid-Ocean Ridge Hydrothermal System

doi: 10.3799/dqkx.2016.036

Huang Wei^{1,2,3
,},
Tao Chunhui^{3,4
,
,},
Li jun¹,
Sun Zhilei¹,
Deng Xiguang²,
Cui Ruyong¹

1.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China
2.
Key Laboratory of Marine Mineral Resources, Ministry of Land and Resources, Guangzhou Marine Geological Survey, Guangzhou 510075, China
3.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China
4.
Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

Received Date: 2015-12-23
Publish Date: 2016-03-15

Abstract

Abstract

The hydrothermal fluids occur along the mid-ocean ridges are capable of transporting a great amount Os from deep interior of the earth where it is relatively enriched to the ocean floor, this process plays a significant role in the global cycling of Os. The geochemical behavior of Os during the various stages of the hydrothermal circulation, its distribution and evolution features and source contributions are estimated basing on the chemical speciation, concentrations and isotopic compositions of Os in the sources for the hydrothermal systems and the hydrothermal deposits. The Os data from the sediment-free mid-ocean ridge systems indicated that there is a nearly complete Os isotope exchange between the interacting seawater and the oceanic crust during the hydrothermal circulation, the behavior of Os appears to be controlled by the relative proportions of seawater and crustal composition in the different tectonic areas. Reactions of seawater with surrounding rock result in the radiogenic Os removing from seawater to the altered host rock, and the nonradiogenic Os lost from the wall rock to the hydrothermal fluid. The hydrothermal deposits accumulated above the seafloor carry Os which is predominately seawater-derived, the Os of the hydrothermal products beneath the the seafloor reflecting mixing of seawater-derived and ocean crust-derived Os.
- Mid-ocean ridge,
- Hydrothermal system,
- Osmium,
- isotopics

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References(57)

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