1887

Abstract

Presented below is a method of the inversion of refraction seismic data. The presentation compares interpretation of refraction data by homogeneous function method with CDP reflection depth section for the same profiles. We show that the method of homogen

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/content/papers/10.3997/2214-4609.201400211
2009-06-08
2021-10-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400211
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