Interseismic strain accumulation across the Manyi fault (Tibet) prior to the 1997 M-w 7.6 earthquake
The coseismic displacements caused by the M w 7.6, 1997 Manyi strike-slip earthquake have been extensively studied. In order to assess whether the current deformation around the Manyi fault is due to one or more postseismic mechanisms and to constrain the rate-state models of afterslip, an estimate...
| Váldodahkkit: | , , |
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| Materiálatiipa: | Journal article |
| Giella: | English |
| Almmustuhtton: |
2011
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