Thermoelastic Stress and Tectonic Evidence in Support of an Initially Totally Molten Moon - or, the "magma Ocean" was 1738KM Deep

Details Thermoelastic Stress and Tectonic Evidence in Support of an Initially Totally Molten Moon - or, the "magma Ocean" was 1738KM Deep Thermoelastic Stress and Tectonic Evidence in Support of an Initially Totally Molten Moon - or, the "magma Ocean" was 1738KM Deep

Mar 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981lpi....12...74b&link_type=gif

LUNAR AND PLANETARY SCIENCE XII, P. 74-76. Abstract.

Physics

Tectonism, Stress, Models, Faults, Moon, Depth

Scientific paper

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