Partial Melting Process in the Upper Mantle Deduced From Morphological and Chemical Variations of the Chromian Spinel Two-Pyroxene Symplectite Due to Progressive Partial Melting of the Horoman Peridotite, Hokkaido, Japan.

JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY
doi 10.2465/ganko.90.93
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Japan Association of Mineralogical Sciences

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