Abstract:
The recently developed method of active vibroseismic monitoring is based on the sounding of a geological structure by seismic waves from artificial controlled sources-vibrators. Thus, the changes occurring in the tensely-deformed state of a medium are considered as related to changes of information parameters of wave fields that are established in the medium with long radiation by the vibrator of broad-band sweep or harmonic signals.
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DOI:
Issue
Pages:
59-64
File:
grigoryuk.pdf
(2.52 MB)