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Abstract

Studying of passive seismicity concerns the physical processes of sound generation by cracks, propagation and recording of elastic waves. One of the main questions remains open - how do radiated elastic waves carry information about physical parameters of their sources (cracks) through a complex geomedium?

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/content/papers/10.3997/2214-4609-pdb.287.1121984
2012-03-04
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1121984
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