Residual displacements and strains due to faulting in real Earth models

Details Residual displacements and strains due to faulting in real Earth models Residual displacements and strains due to faulting in real Earth models

Feb 1974

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974pepi....8...23i&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 8, Issue 1, p. 23-45.

Physics

Scientific paper

Static displacements and strain fields are computed at the free surface of a gravitating radially-heterogeneous earth model. The numerical results indicate that the fields corresponding to a real earth model differ meaningly with comparison to a homogeneous non-gravitating model. The theory is applied to the Alaskan earthquake of March 28, 1964. The strains recorded at Isabella agree with the calculated values; but those at Kippapa and Green Observatory are larger than the theoretical values. In all cases the observed and calculated values are of the same order of magnitude.

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