Abstract
Proposes a method to estimate stress magnitudes in oceanic plate interiors from focal depths and focal mechanisms. Using a depth-dependent rheology, it is possible to estimate the differential stress (σ1-σ3), averaged over some reference lithospheric thickness. The resolving power of the method is investigated by evaluating the effect of uncertainties in parameters that are involved in the analysis. The method is applied to the Central Indian Ocean, where intraplate seismicity is high. From well-studied earthquakes we estimate differential stresses of the order of hundreds of megapascals. -from Authors
Original language | English |
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Journal | Journal of Geophysical Research |
Volume | 97 |
Issue number | B8 |
Publication status | Published - 1992 |