Deformation precursors of the Ust-Barguzin earthquake of May 20, 2008

Instrumental monitoring carried out in geodynamic study regions either directly or indirectly indicates that, at local points of observations, deformations and stresses in the mountainous rocks increase before strong remote earthquakes. They are caused by short tectonic pulses propagating from the s...

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Veröffentlicht in:	Doklady earth sciences 2010-03, Vol.431 (1), p.406-408
1. Verfasser:	Bornyakov, S. A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth and Environmental Science Earth Sciences Earthquakes Geophysics Monitoring systems Mountains Plate tectonics Rock deformation Rocks Seismic activity Seismology
Online-Zugang:	Volltext
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