1887

Abstract

Simultaneously solving for velocity, epsilon, and delta in anisotropic tomography is very challenge. Surface seismic data only is not sufficient for this joint problem. In this work, a model covariance function was built using rock physics to constrain the joint anisotropic tomography. An example from Gulf of Mexico was presented to demonstrate the effectiveness of the method.

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/content/papers/10.3997/2214-4609.20130370
2013-06-10
2020-07-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20130370
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