Depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones
Based on the principle that faults develop where shear stress is maximum, we determine the depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones. Using an elastic half-space model for the south Chile subduction zone, we show that the geometry of a margin-para...
Αποθηκεύτηκε σε:
| Εκδόθηκε σε: | Andean Geology |
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| Κύριοι συγγραφείς: | , , , |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Servicio Nacional de Geología y Minería
2017
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| Θέματα: | |
| Διαθέσιμο Online: | https://www.redalyc.org/articulo.oa?id=173949489005 https://www.redalyc.org/journal/1739/173949489005/ https://www.redalyc.org/journal/1739/173949489005/html/ https://www.redalyc.org/journal/1739/173949489005/173949489005.epub https://www.redalyc.org/journal/1739/173949489005/movil |
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