Physics
Scientific paper
Mar 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994em%26p...64..265b&link_type=abstract
Earth, Moon, and Planets, vol. 64, no. 3, p. 265-271
Physics
Deformation, Earth Tides, Earth-Moon System, Ellipsoids, Flattening, Lunar Equator, Lunar Gravitation, Lunar Rotation, Lunar Tides, Lunar Topography, Mapping, Moon, Surface Distortion, Earth (Planet), Harmonic Analysis, Legendre Functions, Mass, Orbital Mechanics, Radii, Shapes
Scientific paper
The second zonal and the second sectorial Stokes parameters of the Moon's gravitational field and/or polar and equatorial flattenings of the lunar triaxial level ellipsoid have been explained by the tidal and rotational distortions due to the Earth. The Epoch at which the Moon's figure formation was finished has been estimated as 1.6 x 109 y B. P. when the Earth-Moon distance was about 168 400 km and the orbital/rotational period of the Moon about 8 days.
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