Recycled lower continental crust: Re-Os isotopic evidence from peridotite xenoliths entrained by Mesozoic high-Mg diorites in the eastern North China Craton

Details Recycled lower continental crust: Re-Os isotopic evidence from peridotite xenoliths entrained by Mesozoic high-Mg diorites in the eastern North China Craton Recycled lower continental crust: Re-Os isotopic evidence from peridotite xenoliths entrained by Mesozoic high-Mg diorites in the eastern North China Craton

Jun 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009gecas..73q1465x&link_type=openurl

Geochimica et Cosmochimica Acta Supplement, Volume 73, p.A1465

Physics

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