Dynamics of a fault model with two mechanically different regions
Abstract We consider a fault containing two regions with different mechanical behaviours: a strong, velocity-weakening region (asperity) and a weak, velocity-strengthening region. The fault is embedded in a shear zone subject to a constant strain rate by the motions of adjacent tectonic plates. The...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
SpringerOpen
2017-10-01
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Series: | Earth, Planets and Space |
Subjects: | |
Online Access: | http://link.springer.com/article/10.1186/s40623-017-0731-2 |