Source and magma mixing processes in continental subduction factory: Geochemical evidence from postcollisional mafic igneous rocks in the Dabie orogen-Reference-Cited by-同舟云学术

Source and magma mixing processes in continental subduction factory: Geochemical evidence from postcollisional mafic igneous rocks in the Dabie orogen

Published:2015-03 Issue:3 Volume:16 Page:659-680
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Dai Li-Qun¹,Zhao Zi-Fu¹,Zheng Yong-Fei¹,Zhang Juan²

Affiliation:

1. CAS Key Laboratory of Crust-Mantle Materials and Environments; School of Earth and Space Sciences, University of Science and Technology of China; Hefei China

2. State key Laboratory of Continental Dynamics, Department of Geology; Northwest University; Xi'an China

Funder

Chinese Ministry of Science and Technology

Natural Science Foundation of China

Fundamental Funds for the Central Universities

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference86 articles.

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2. Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: Nature, origin, and relations with the hosts;Barbarin;Lithos,2005