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ON THE CORRELATION OF GRAVITY WITH TIDAL ANOMALIES *
Author(s) -
GROTEN E.
Publication year - 1964
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1964.tb01915.x
Subject(s) - geology , geophysics , gemology , spherical harmonics , gravity anomaly , geodesy , post glacial rebound , gravitational field , regional geology , harmonics , mantle (geology) , isostasy , seismology , sea level , physics , volcanism , tectonics , engineering geology , oceanography , lithosphere , paleontology , classical mechanics , quantum mechanics , voltage , oil field
Tidal deformations of the solid earth show remarkable regional fluctuations. Mean gravity anomalies reveal strong positive correlation with the regional variations in the vertical tide component, if the effect of topography on the gravity field is reduced by isostatic proceedings. The correlation of these “tidal anomalies” with the lower harmonics of the gravity field is weaker. Heterogenities of the upper mantle may be a source of these differences in the deformations.

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