Highly refractory peridotites in Songshugou, Qinling orogen: Insights into partial melting and melt/fluid–rock reactions in forearc mantle-Reference-Cited by-同舟云学术

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Highly refractory peridotites in Songshugou, Qinling orogen: Insights into partial melting and melt/fluid–rock reactions in forearc mantle

Published:2016-05 Issue: Volume:252-253 Page:234-254
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Cao Yi,Song Shuguang,Su Li,Jung Haemyeong,Niu Yaoling

Funder

Major State Basic Research Development Projects

National Natural Science Foundation of China

NRF

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference112 articles.

1. Carbon dioxide released from subduction zones by fluid-mediated reactions;Ague;Nature Geoscience,2014

2. Chemistry of chromian spinel in volcanic-rocks as a potential guide to magma chemistry;Arai;Mineralogical Magazine,1992

3. Characterization of spinel peridotites by olivine–spinel compositional relationships: review and interpretation;Arai;Chemical Geology,1994

4. Podiform chromitites of the Tari–Misaka ultramafic complex, southwestern Japan, as mantle–melt interaction products;Arai;Economic Geology,1994

5. Concentration of incompatible elements in oceanic mantle: effect of melt/wall interaction in stagnant or failed melt conduits within peridotite;Arai;Geochimica et Cosmochimica Acta,1997

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