Articulo
Tectonic role of margin-parallel and margin-transverse faults during oblique subduction in the Southern Volcanic Zone of the Andes: Insights from Boundary Element Modeling.
Fecha
2016Registro en:
15090013
WOS:000385861300001
no scielo
eid=2-s2.0-84985905590
Institución
Resumen
Obliquely convergent subduction margins develop trench‐parallel faults shaping the regional architecture of orogenic belts and partitioning intraplate deformation. However, transverse faults also are common along most orogenic belts and have been largely