Connection between variations of the stress-strain state of the Earth’s crust and seismic activity: The example of Southern California
A three-dimensional geomechanical model of Southern California, including mountain relief, fault tectonics, and characteristic internal borders, such as the roof of the consolidated crust and Moho surface, was created. The initial stress state of the model is determined by the gravitational force an...
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| Veröffentlicht in: | Doklady earth sciences 2010, Vol.430 (1), p.147-150 |
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| container_title | Doklady earth sciences |
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| creator | Bondur, V. G. Garagash, I. A. Gokhberg, M. B. Lapshin, V. M. Nechaev, Yu. V. |
| description | A three-dimensional geomechanical model of Southern California, including mountain relief, fault tectonics, and characteristic internal borders, such as the roof of the consolidated crust and Moho surface, was created. The initial stress state of the model is determined by the gravitational force and horizontal tectonic movement, established on basis of GPS observations. Monitoring of variations in the stress state of the Earth’s crust and lithosphere, which are generated by seismic processes, has shown that the model enables us to predict an increase of seismic activity in a region and to mark the places in which average earthquakes can occur in the following two weeks. |
| doi_str_mv | 10.1134/S1028334X10010320 |
| format | Article |
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| ispartof | Doklady earth sciences, 2010, Vol.430 (1), p.147-150 |
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| subjects | Analysis Crust Earth Earth and Environmental Science Earth Sciences Earthquakes Geophysics Global positioning systems GPS Gravity Lithosphere Plate tectonics Seismic activity Seismology Stress-strain curves Tectonics Tectonics (Geology) |
| title | Connection between variations of the stress-strain state of the Earth’s crust and seismic activity: The example of Southern California |
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