1887

Abstract

We consider signal propagation in one layer with a constant velocity-gradient: layer in which the signal velocity increases linearly with depth. We use the traveltime and the four derivatives of the traveltime with respect to the locations of the source a

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/content/papers/10.3997/2214-4609.201400165
2009-06-08
2021-12-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400165
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