3-D ray-tracing in anisotropic media , by Jean Luc Guiziou

The issue of adapting a fast 3-D seismic ray-tracing algorithm to anisotropic media is addressed. Two approaches are considered. A method restricted to orthotropic anisotropy leads to exact calculations of traveltimes. A second algorithm, based on linearization techniques, enables to approximate the traveltimes in the case of an inhomogeneous generally anisotropic medium, under the assumption of weak anisotropy. The two methods are discussed in terms of their potential application to reflection seismology.


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