Deep vs. Shallow Origin of Gravity Anomalies and Topography on the Moon

Details Deep vs. Shallow Origin of Gravity Anomalies and Topography on the Moon Deep vs. Shallow Origin of Gravity Anomalies and Topography on the Moon

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1694s&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1694

Computer Science

Scientific paper

If density anomalies in both viscous mantle and elastic lithosphere can
be modelled as "white noise", we can compute the "expected" lunar geoid
spectrum and explain degrees 2-5 including the flattening term, as
mainly due to mantle density anomalies.

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