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1 Department of
Geosciences
Princeton University
Princeton, New Jersey
08544
(J.-P.A.)
* Present address: Institute of Geophysics, Seismology, and Geodynamics, ETH Hönggerberg (HPP), CH-8093 Zürich, Switzerland; ampuero{at}erdw.ethz.ch.
An earthquake on a fault separating two dissimilar materials does not have a well-defined moment density tensor. We present a complete characterization of this bimaterial ambiguity in the general case of slip on a fault in an anisotropic medium. The ambiguity can be eliminated by utilizing a potency density rather than a moment density representation of a bimaterial source.
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