1887

Abstract

This paper presents the interpretation of reflections from same very shallow fracture zones located at the depth of less than 250m and recorded in soundings carried out on bedrock outcrops and in boreholes. The resolution of the seismic reflection method is compared to the corresponding acoustic logs and other geophysical and geological investigations.

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/content/papers/10.3997/2214-4609.201410972
1991-05-28
2020-07-12
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