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Transpressional tectonics and strain partitioning during oblique collision between three plates in the Precambrian of southeast Brazil
(1998-12-01)
This paper is part of the special publication Continental transpressional and transtensional tectonics (eds R.E. Holdsworth, R.A. Strachan and J.F. Dewey). Two orogenic belts have been recognized in south- east Brazil, ...
Partição de deformação em aços dual-phase
(Universidade Federal de Minas GeraisBrasilENG - DEPARTAMENTO DE ENGENHARIA METALÚRGICAPrograma de Pós-Graduação em Engenharia Metalúrgica, Materiais e de MinasUFMG, 2022-09-29)
The tailoring of new alloys often requires improvement in strength, for performance, and ductility to support mechanical processing until the final shape is achieved. Important advances have been obtained in the last decades ...
Transpressional tectonics and strain partitioning during oblique collision between three plates in the Precambrian of southeast Brazil
(1998-12-01)
This paper is part of the special publication Continental transpressional and transtensional tectonics (eds R.E. Holdsworth, R.A. Strachan and J.F. Dewey). Two orogenic belts have been recognized in south- east Brazil, ...
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 ...
Kinematic variations across Eastern Cordillera at 24°S (Central Andes): tectonic and magmatic implications
(Elsevier Science, 2007-04)
The Eastern Cordillera (Central Andes, ∼ 24°S) consists of a basement-involved thrust system, resulting from Miocene-Quaternary eastward migrating compression, separating the Puna plateau from the Santa Barbara System ...