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...
Uloženo v:
| Vydáno v: | Andean Geology |
|---|---|
| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Servicio Nacional de Geología y Minería
2017
|
| Témata: | |
| On-line přístup: | 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 |
| Tagy: |
Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!
|