Early Paleozoic high-Mg granodiorite from the Erlangping unit, North Qinling orogen, central China: Partial melting of metasomatic mantle during the initial back-arc opening-Reference-Cited by-同舟云学术

Early Paleozoic high-Mg granodiorite from the Erlangping unit, North Qinling orogen, central China: Partial melting of metasomatic mantle during the initial back-arc opening

Published:2017-09 Issue: Volume:288-289 Page:282-294
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Abdallsamed Mohammed I.M.,Wu Yuan-Bao,Zhang Wenxiang,Zhou Guangyan,Wang Hao,Yang Saihong

Funder

Ministry of Science and Technology of China

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference97 articles.

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5. Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting, mantle and crustal, sources? A review;Bonin;Lithos,2004

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