Re–Os isotope geochronology of the Shangbao pyrite–flourite deposit in southeastern Hunan, South China: Evidence for multiple mineralization events and the role of crust–mantle interaction in polymetallic deposits-Reference-Cited by-同舟云学术

Re–Os isotope geochronology of the Shangbao pyrite–flourite deposit in southeastern Hunan, South China: Evidence for multiple mineralization events and the role of crust–mantle interaction in polymetallic deposits

Published:2017-12 Issue:4 Volume:2 Page:109-122
ISSN:2451-912X
Container-title:Solid Earth Sciences
language:en
Short-container-title:Solid Earth Sciences

Author:

Huang Cheng-Cheng,Guo Hai-Feng,Li Jie,Wang Qiang,Zhang Chunfu,Wyman Derek,Tang Gong-Jian

Funder

DREAM Program of China

Key Program of the Chinese Academy of Sciences

Strategic Priority Research Program (B) of the Chinese Academy of Sciences

National Natural Science Foundation of China

Talent Project of Guangdong Province

GIGCAS 135 project

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geochemistry and Petrology,Geology,Geophysics,Geotechnical Engineering and Engineering Geology

Reference105 articles.

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3. Re–Os isotopic measurements at the femtomole level in natural samples;Birck;Geostand. Newsl.,1997

4. Diffusion of osmium in pyrrhotite and pyrite implications for closure of the Re–Os isotopic system;Brenan;Earth Planet. Sci. Lett.,2000

5. Re–Os systematics of pyrite from the Bolcana porphyry copper deposit, Apuseni Mountains, Romania;Cardon;Econ. Geol.,2008

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