Mineral-aqueous fluid partitioning of trace elements at 900--1200dC and 3.0--5.7 GPa: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism

Details Mineral-aqueous fluid partitioning of trace elements at 900--1200dC and 3.0--5.7 GPa: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism Mineral-aqueous fluid partitioning of trace elements at 900--1200dC and 3.0--5.7 GPa: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism

May 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998gecoa..62.1781s&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 62, p. 1781-1801.

Physics

52

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