Platinum-group element abundances and Re–Os isotopic systematics of the upper continental crust through time: Evidence from glacial diamictites-Reference-Cited by-同舟云学术

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Platinum-group element abundances and Re–Os isotopic systematics of the upper continental crust through time: Evidence from glacial diamictites

Published:2016-10 Issue: Volume:191 Page:1-16
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Chen Kang,Walker Richard J.,Rudnick Roberta L.,Gao Shan,Gaschnig Richard M.,Puchtel Igor S.,Tang Ming,Hu Zhao-Chu

Funder

National Science Foundation

National Nature Science Foundation of China

Chinese Ministry of Education

State Key Laboratory of Geological Processes and Mineral Resources

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference67 articles.

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2. Rhenium in seawater: confirmation of generally conservative behavior;Anbar;Geochim. Cosmochim. Acta,1992

3. Tracking the budget of Nb and Ta in the continental crust;Barth;Chem. Geol.,2000

4. Highly siderophile element composition of the Earth’s primitive upper mantle: constraints from new data on peridotite massifs and xenoliths;Becker;Geochim. Cosmochim. Acta,2006

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

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