A thermo-chemical regime in the upper mantle in the early Earth inferred from a numerical model of magma-migration in a convecting upper mantle

Details A thermo-chemical regime in the upper mantle in the early Earth inferred from a numerical model of magma-migration in a convecting upper mantle A thermo-chemical regime in the upper mantle in the early Earth inferred from a numerical model of magma-migration in a convecting upper mantle

Apr 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996pepi...94..187k&link_type=ejournal

Physics of the Earth and Planetary Interiors, v. 94, p. 187-215

Physics

7

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