Open-and Closed-System Magma Evolution of Apollow 17 High-Ti Basalts and Origin of Source Heterogeneities at 4.1 Ga: Sr-Nd Isotopic Evidence

Details Open-and Closed-System Magma Evolution of Apollow 17 High-Ti Basalts and Origin of Source Heterogeneities at 4.1 Ga: Sr-Nd Isotopic Evidence Open-and Closed-System Magma Evolution of Apollow 17 High-Ti Basalts and Origin of Source Heterogeneities at 4.1 Ga: Sr-Nd Isotopic Evidence

Mar 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990lpi....21..926p&link_type=gif

Abstracts of the Lunar and Planetary Science Conference, volume 21, page 926, (1990)

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