Trace elements in olivine: Proxies for petrogenesis, mineralization and discrimination of mafic-ultramafic rocks-Reference-Cited by-同舟云学术

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Trace elements in olivine: Proxies for petrogenesis, mineralization and discrimination of mafic-ultramafic rocks

Published:2021-05 Issue: Volume:388-389 Page:106085
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Wang Jing,Su Ben-Xun,Robinson Paul T.,Xiao Yan,Bai Yang,Liu Xia,Sakyi Patrick Asamoah,Jing Jie-Jun,Chen Chen,Liang Zi,Bao Zhi-An

Funder

Chinese Academy of Sciences Youth Innovation Promotion Association

Youth Innovation Promotion Association

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference84 articles.

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2. The sublithospheric mantle as the source of continental flood basalts; the case against the continental lithosphere and plume head reservoirs;Anderson;Earth Planet. Sci. Lett.,1994

3. Base metal mineral segregation and Fe-Mg exchange inducing extreme compositions of olivine and chromite from the Xiadong Alaskan-type complex in the southern part of the Central Asian Orogenic Belt;Bai;Ore Geol. Rev.,2017

4. Diffusion-driven chromium isotope fractionation in ultramafic cumulate minerals: elemental and isotopic evidence from the Stillwater complex;Bai;Geochim. Cosmochim. Acta,2019

5. Magnesium and iron isotopic evidence of inter-mineral diffusion in ultramafic cumulates of the Peridotite Zone, Stillwater Complex;Bai;Geochim. Cosmochim. Acta,2021

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