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Oblique subduction and strain partitioning: Tectonic role of margin-parallel and margin-transverse structures at the Southern Volcanic Zone of the Andes
(2015)
Convergent margins undergoing oblique subduction develop margin-parallel structural domains, which accommodate the long-term crustal deformation within the overriding plate. Although the Andes are no exception, ...
Nature of crustal deformation arising from oblique subduction: Strain Partitioning, Strike-Slip Faulting and S
(2015)
The Chilean margin is characterized by the oblique subduction of the Nazca plate beneath the South American plate at a rate of 66 mm/yr. Most of the deformation arising from this tectonic regime is taken up by slip at the ...
Deformational evolution of a Cretaceous subduction complex: Elephant Island, South Shetland Islands, Antarctica
(Elsevier B.V., 2000-03-30)
New structural data from Elephant Island and adjacent islands are presented with the objective to improve the understanding of subduction kinematics in the area northeast of the Antarctic Peninsula. on the island, a first ...
Deformational evolution of a Cretaceous subduction complex: Elephant Island, South Shetland Islands, Antarctica
(Elsevier B.V., 2000-03-30)
New structural data from Elephant Island and adjacent islands are presented with the objective to improve the understanding of subduction kinematics in the area northeast of the Antarctic Peninsula. on the island, a first ...
Depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones
(2017)
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 ...
Depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones
(2017)
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 ...