Origin of Geochemical Heterogeneity in the Mantle Peridotites from the Bay of Islands Ophiolite, Newfoundland, Canada: Ion Probe Study of Clinopyroxenes

Details Origin of Geochemical Heterogeneity in the Mantle Peridotites from the Bay of Islands Ophiolite, Newfoundland, Canada: Ion Probe Study of Clinopyroxenes Origin of Geochemical Heterogeneity in the Mantle Peridotites from the Bay of Islands Ophiolite, Newfoundland, Canada: Ion Probe Study of Clinopyroxenes

Mar 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998gecoa..62..853b&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 62, p. 853-866.

Physics

14

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