Geochronology, Geochemistry, and Hf Isotopic Compositions of Monzogranites and Mafic-Ultramafic Complexes in the Maxingdawannan Area, Eastern Kunlun Orogen, Western China: Implications for Magma Sources, Geodynamic Setting, and Petrogenesis-Reference-Cited by-同舟云学术

Geochronology, Geochemistry, and Hf Isotopic Compositions of Monzogranites and Mafic-Ultramafic Complexes in the Maxingdawannan Area, Eastern Kunlun Orogen, Western China: Implications for Magma Sources, Geodynamic Setting, and Petrogenesis

Published:2019-04 Issue:2 Volume:30 Page:335-347
ISSN:1674-487X
Container-title:Journal of Earth Science
language:en
Short-container-title:J. Earth Sci.

Author:

Yan Jiaming^ORCID,Sun Guosheng^ORCID,Sun Fengyue,Li Liang,Li Haoran,Gao Zhenhua,Hua Lei,Yan Zhengping

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s12583-018-1203-8.pdf

Reference95 articles.

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4. Campbell, I. H., 2002. Implications of Nb/U, Th/U and Sm/Nd in Plume Magmas for the Relationship between Continental and Oceanic Crust Formation and the Development of the Depleted Mantle. Geochimica et Cosmochimica Acta, 66(9): 1651–1661. https://doi.org/10.1016/s0016-7037(01)00856-0

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