Plagioclase Dissolution in the Lunar Magma Ocean: A New Model for the Origin of Lunar Ferroan Anorthosites and the Rapid Growth of Highlands Crust

Details Plagioclase Dissolution in the Lunar Magma Ocean: A New Model for the Origin of Lunar Ferroan Anorthosites and the Rapid Growth of Highlands Crust Plagioclase Dissolution in the Lunar Magma Ocean: A New Model for the Origin of Lunar Ferroan Anorthosites and the Rapid Growth of Highlands Crust

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1029s&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1029

Physics

Scientific paper

A new model for the rapid formation of lunar highlands crust which
explains the negative slope of the ferroan anorthsite suite on the Fo-An
diagram.

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