Metallic iron in the bottom regions of lunar mare /possible interpretation of geophysical data/

Details Metallic iron in the bottom regions of lunar mare /possible interpretation of geophysical data/ Metallic iron in the bottom regions of lunar mare /possible interpretation of geophysical data/

Sep 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980dossr.254..959k&link_type=abstract

Akademiia Nauk SSSR, Doklady, vol. 254, no. 4, 1980, p. 959-962. In Russian.

Physics

Iron, Lunar Composition, Lunar Maria, Lunar Rocks, Basalt, Geochemistry, Lunar Geology

Scientific paper

The interface of the mare basalt (or megaregolith, in the absence of the
latter) and the primitive rock is of distinct interest to the
understanding of mare geology. The present discussion of available
geophysical data and the geochemical properties of lunar rocks indicates
that the interface region must be rich in metallic iron.

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