Data for: Origin of high-Cr chromite deposits in nascent mantle wedges: Petrological and geochemical constraints from the Neo-Tethyan Luobusa ophiolite, Tibet

Published: 25 May 2020| Version 1 | DOI: 10.17632/n8zjdr6dbg.1
Contributors:
Pengfei Zhang,
John Malpas,
Mei-Fu Zhou,
Paul Robinson

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The uploaded tables above are supplementary to our manuscript, titled "Origin of high-Cr chromite deposits in nascent mantle wedges: Petrological and geochemical constraints from the Neo-Tethyan Luobusa ophiolite, Tibet". Table-S1 presents the EPMA data of chromite obtained in this study. Table-S2 presents the complied major element compositions of clinopyroxene in peridotites and chromitites from previous studies. Table-S3 presents the complied REE compositions of clinopyroxene in the cpx-rich and cpx-poor harzburgites from previous studies. Table-S4 presents the complied REE compositions of harzburgites and dunites from previous studies. Table-S5 presents the calculated REE compositions of the parental melts of clinopyroxene grains in the Luobusa harzburgites. Detailed sources of the complied data have been given in the Table-S2 to Table-S5.

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Economic Geology, Geochemistry

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