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Stress-strain state assessment of seismotectonic activity zones by the kinematic parameter
1 Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia
2 Republic Center of Seismological Service of Azerbaijan National Academy of Sciences, Baku, Azerbaijan
2 Republic Center of Seismological Service of Azerbaijan National Academy of Sciences, Baku, Azerbaijan
Journal: Problems of Engineering Seismology
Tome: 44
Number: 1
Year: 2017
Pages: 31-56
UDK: 550.34
DOI: 10.21455/VIS2017.1-2
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Slavina L., Kuchau M., Likhodeev D., Abdullaeva R. Stress-strain state assessment of seismotectonic activity zones by the kinematic parameter // . 2017. Т. 44. № 1. С. 31-56. DOI: 10.21455/VIS2017.1-2
@article{SlavinaStress-strain2017,
author = "Slavina, L. and Kuchau, M. and Likhodeev, D. and Abdullaeva, R.",
title = "Stress-strain state assessment of seismotectonic activity zones by the kinematic parameter ",
journal = "Problems of Engineering Seismology",
year = 2017,
volume = "44",
number = "1",
pages = "31-56",
doi = "10.21455/VIS2017.1-2",
language = "English"
}
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Keywords: seismic wave velocity ratio, stress field
Аnnotation: Earthquakes occur as a result of tectonic movements in the bowels of the Earth and contain information about spatio-temporal changes in the stress-strain state of the Earth's crust. In particular, an increase in the activity of weak earthquakes indicates the general activation of a section of the seismotectonic zone and nucleation of a strong event. Monitoring the travel times of P - and S -waves and the ratio of their velocities (parameter V
