Possible reduction of earthquake hazard on the Wellington Fault, New Zealand, after the nearby 1855, M 8.2 Wairarapa earthquake and implication for interpreting paleoearthquake intervals
Based on the indicative modelling, the changes in Coulomb failure function (?CFS) suggest that the W-HV segment and the T-P segment could be stable in at least the future 300 years and 190 years respectively, for these periods should be needed to accumulate the stress released by the M 8.2...
Αποθηκεύτηκε σε:
| Κύριος συγγραφέας: | |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
2003-06-01
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| Σειρά: | Annals of Geophysics |
| Θέματα: | |
| Διαθέσιμο Online: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3450 |
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