The Influence of Tidal, Despinning, and Magma Ocean Cooling Stresses on the Magnitude and Orientation of the Moon's Early Global Stress Field

Details The Influence of Tidal, Despinning, and Magma Ocean Cooling Stresses on the Magnitude and Orientation of the Moon's Early Global Stress Field The Influence of Tidal, Despinning, and Magma Ocean Cooling Stresses on the Magnitude and Orientation of the Moon's Early Global Stress Field

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1542s&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1542

Physics

Scientific paper

We address the influence tidal, de-spinning, and magma ocean cooling
stresses have on the global stress field of a growing lunar crust.
Surface extensional and strike-slip features are evident. Strike-slip
faulting operates to great crustal depths.

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