Heterogeneous mantle beneath the Neo-Tethys Ocean revealed by ultramafic rocks from the Xiugugabu Ophiolite in the Yarlung-Tsangpo Suture Zone, southwestern Tibet-Reference-Cited by-同舟云学术

Heterogeneous mantle beneath the Neo-Tethys Ocean revealed by ultramafic rocks from the Xiugugabu Ophiolite in the Yarlung-Tsangpo Suture Zone, southwestern Tibet

Published:2023-08 Issue:8 Volume:178 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Zhang Chang^ORCID,Liu Chuan-Zhou,Bénard Antoine,Müntener Othmar,Ji Wen-Bin,Liu Tong,Zhang Zhen-Yu,Zhang Wei-Qi,Wu Fu-Yuan

Funder

China National Funds for Distinguished Young Scientists

Key Technologies Research and Development Program

Key Research Program of the Institute of Geology and Geophysics, CAS

National Natural Science Foundation of China

China Scholarship Council

European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00410-023-02039-3.pdf

Reference131 articles.

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5. Ballhaus C, Berry RF, Green DH (1991) High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle. Contrib Miner Petrol 107:27–40

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