ANOMALIES OF DENSITY, STRESSES, AND GRAVITY IN THE INTERIOR OF EARTH AND MARS AND POSSIBLE GEODINAMI

来源 :International Symposium & Summer School on Planetary Science | 被引量 : 0次 | 上传用户:acdef2
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  Formulas that include in the quadratic approximation the contribution of anomalous masses, distributed in height to the reference ellipsoid, to the Stokes constant have been derived.It is shown that the contribution of the quadratic terms is especially important in the case of dipole (by height) distribution of anomalous masses and it is compared in order of magnitude to the linear contribution.
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