Formation of hybrid mantle pyroxenites by reaction between mafic layer-derived melts and peridotites: Implications for OIB source heterogeneity

Details Formation of hybrid mantle pyroxenites by reaction between mafic layer-derived melts and peridotites: Implications for OIB source heterogeneity Formation of hybrid mantle pyroxenites by reaction between mafic layer-derived melts and peridotites: Implications for OIB source heterogeneity

Jun 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009gecas..73q.293d&link_type=openurl

Geochimica et Cosmochimica Acta Supplement, Volume 73, p.A293

Physics

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