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the geochemical modelisation of assimilation of preexisting gabbroic rocks by plume-derived melts could explain the characteristics of the Kerguelen OIBs
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This page is a summary of: Origin of primitive ocean island basalts by crustal gabbro assimilation and multiple recharge of plume-derived melts, Geochemistry Geophysics Geosystems, July 2017, American Geophysical Union (AGU),
DOI: 10.1002/2017gc006986.
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