1887

Abstract

Zones of permafrast down to 500 m in some regions of Western and Eastern Siberia cause specific distribution of elastic wave velocities in overburden which becomes especially apparent in sand-clay rocks. In generally observed increased velocities extensive zones of velocity decrease exist resulting in considerable distortions of different events arrival times, arriving from deeper horizons.

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/content/papers/10.3997/2214-4609.201409434
1995-05-29
2021-06-14
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409434
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