1887

Abstract

Cross-hole seismic data are usually processed and interpreted by ignoring the presence of the borehole i .e., by assuming that the sources and receivers are simply buried in the subsurface . This assumption is generally acceptable for ray tomography methods using first arrivals only, but must be revised in diffraction or full waveform tomography techniques.

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/content/papers/10.3997/2214-4609.201410425
1992-06-01
2020-11-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410425
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