Abstract
AbstractIn this paper, we analyse how the combination of fault zone shape and material properties affects the propagation of seismic waves in a two-dimensional domain. We focus on SH wave propagation through several faults with different thicknesses and bending radii, but the theory is easily generalized to the three-dimensional case. We show how the density of energy released is mostly a function of the radius and does not depend on the velocity inside a fault zone.
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Cited by
3 articles.
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