Abstract
Earthquakes have been recognized as resulting from stick-slip frictional instabilities along the faults between deformable rocks. A three-dimensional finite-element code for modeling the nonlinear frictional contact behaviors between deformable bodies with the node-to-point contact element strategy has been developed and applied here to investigate the fault geometry influence on the nucleation and development process of the stick-slip instability along an intra-plate fault through a typical fault bend model, which has a pre-cut fault that is artificially bent by an angle of 5.6° at the fault center. The numerical results demonstrate that the geometry of the fault significantly affects nucleation, termination and restart of the stick-slip instability along the intra-plate fault, and all these instability phenomena can be well simulated using the current finite-element algorithm.
| Original language | English |
|---|---|
| Pages (from-to) | 2091-2102 |
| Number of pages | 12 |
| Journal | Pure and Applied Geophysics |
| Volume | 161 |
| Issue number | 9-10 |
| DOIs | |
| State | Published - Oct 2004 |
| Externally published | Yes |
Keywords
- Earthquake
- Fault bends
- Finite-element method
- Friction instability
- Frictional contact between deformable bodies
- Stick-slip instability
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
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