Co2+ as a chemical analogue for Fe2+ in high-temperature experiments in basaltic systems

Details Co2+ as a chemical analogue for Fe2+ in high-temperature experiments in basaltic systems Co2+ as a chemical analogue for Fe2+ in high-temperature experiments in basaltic systems

May 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976e%26psl..30..303c&link_type=ejournal

Earth and Planetary Science Letters, Vol. 30, p.303

Physics

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