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...
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Autores principales: | Catalán,Nicole, Bataille,Klaus, Tassara,Andrés, Araya,Rodolfo |
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Lenguaje: | English |
Publicado: |
Servicio Nacional de Geología y Minería (SERNAGEOMIN)
2017
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Acceso en línea: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062017000100005 |
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