2006
DOI: 10.1134/s1028334x06030287
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Geoacoustic location of earthquake preparation areas

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Cited by 9 publications
(3 citation statements)
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“…Seismic activity in arctic latitudes under an ice layer is accompanied by acoustic deformation of ice cover [1]. Acoustic elastic waves occur in an ice layer in the rage from units to tens of kHz [2,3,4,5]. In order to record earthquake sources deep under the water and far away from an ice edge, we need to develop mathematical models for the processes of elastic acoustic wave propagation at the boundary of water and ice.…”
Section: Introductionmentioning
confidence: 99%
“…Seismic activity in arctic latitudes under an ice layer is accompanied by acoustic deformation of ice cover [1]. Acoustic elastic waves occur in an ice layer in the rage from units to tens of kHz [2,3,4,5]. In order to record earthquake sources deep under the water and far away from an ice edge, we need to develop mathematical models for the processes of elastic acoustic wave propagation at the boundary of water and ice.…”
Section: Introductionmentioning
confidence: 99%
“…Among the preseismic anomalies of the near-surface fields, increase of high-frequency geoacoustic emission in kilohertz frequency range [5][6][7][8][9] and bay-like decrease of atmospheric electric field with sign change during calm weather conditions [10][11][12][13][14][15] are observed. Anomalies of these fields, essentially different, occur in solid and air mediums and have different polarity that indicates various mechanisms of formation.…”
Section: Introductionmentioning
confidence: 99%
“…The paper [1] experimentally proves that deformation-acoustic activity which appears before earthquakes may be considered as a complex precursor of a seismic event. One of the methods to record earthquake precursors is the method of acoustic elastic wave recording in the range from 0 to 10 kHz in small water pools [2][3][4][5].…”
Section: Introductionmentioning
confidence: 99%