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- W3196543168 abstract "The block-and-fault dynamics model was developed using the following assumptions: a region is a structure of perfectly rigid blocks separated by infinitely thin flat faults; all deformations occur in fault planes and on the block bottoms. Blocks move as a consequence of a prescribed movement of the structure boundaries and the underlying medium. The displacements of the blocks are determined so that the structure is in a quasi-static equilibrium state. The interaction of blocks along the fault planes is viscous-elastic, as long as the ratio of stress to pressure remains below a certain strength level. When this critical level is exceeded, a stress-drop (“failure”) occurs. These failures are considered as earthquakes. A review of the results obtained by numerically simulating for various block structures is given, including the results recently obtained for the Altai-Sayany-Baikal region. The use of the model for seismic hazard assessment is discussed." @default.
- W3196543168 created "2021-09-13" @default.
- W3196543168 creator A5051457283 @default.
- W3196543168 date "2022-01-01" @default.
- W3196543168 modified "2023-09-27" @default.
- W3196543168 title "Modeling the block-and-fault structure dynamics with application to studying seismicity and geodynamics" @default.
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- W3196543168 doi "https://doi.org/10.1016/b978-0-12-823503-4.00004-x" @default.
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