1887

Abstract

Small scale structures with velocity anomalies of a few percent are often the targets of the seismic travel time tomography between boreholes or tunnels. To successfully invert for these velocity structures, accurate knowledge of the source and receiver coordinates and of the shot times is required.

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/content/papers/10.3997/2214-4609.201407440
1995-09-25
2020-09-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407440
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