Deformation and acoustic precursors of earthquakes

An increase in the intensity of high-frequency geoacoustic emission in near-surface sedimentary rocks during the final stage of earthquake preparation at a significant distance from their epicenters is caused by an increase in local stresses [13]. Variations in the stresses related to the effect men...

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Veröffentlicht in:	Doklady earth sciences 2007-03, Vol.413 (1), p.281-285
Hauptverfasser:	Dolgikh, G. I., Kuptsov, A. V., Larionov, I. A., Marapulets, Yu. V., Shvets, V. A., Shevtsov, B. M., Shirokov, O. P., Chupin, V. A., Yakovenko, S. V.
Format:	Artikel
Sprache:	eng
Schlagworte:	Acoustics Deformation Earth sciences Earthquakes Plate tectonics Precursors Rock deformation Sedimentary rocks Seismic activity Seismic phenomena Seismology
Online-Zugang:	Volltext
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