"Deformação polifásica e metamorfismo do Grupo Cuiabá na região de Poconé (MT), cinturão de dobras e cavalgamentos Paraguai"

• Autor(a) principal: Vasconcelos, Bruno Rodrigo
• Data de Publicação: 2014
• Tipo de documento: Dissertação
• Idioma: por
• Título da fonte: Repositório Institucional da UFMT
• Texto Completo: http://ri.ufmt.br/handle/1/590
• topic: Cinturão de dobras e cavalgamento Paraguai; Geologia estrutural; Metamorfismo; CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS; Paraguay fold and thrust belt; Structural geology; Metamorphism

Several deformation models have been proposed for the Paraguay Belt, differing mainly in the number of deformation phases, sense of vergence and tectonic style. Structural features presented in this work indicate tectonic dominated by an initial phase of low dipping thrust sheets, followed by two progressive deformation phases. The first deformation phase (F1) is characterized by a slaty cleavage (S1), axial plane of isoclinal recumbent folds (D1) in the NE direction, with recrystallization of minerals from the greenschist facies, related to horizontal shear zones with top-to-the-SE sense of movement. The second stage shows a NW-vergence, characterized by crenulation cleavage, S0 and S1 axial planes of open folds, locally associated with reverse faults. The third deformation phase is characterized by subvertical faults and fractures in the NW direction showing sinistral movement, commonly filled by quartz veins. The collection of tectonic structures and metamorphic paragenesis described indicate that the most intense deformation, at deeper crustal level, reached the greenschist facies during F1. Accommodating significant crustal shortening through isoclinal recumbent folds and low-angle shear zones showing top-to-the SE sense of movement during a thin-skinned tectonic regime. The phase F2 showed more subtle deformation, with more competent rock types developing brittle behavior and less competent rock types developing ductile behavior, by accommodating slight shortening through normal open folds and subvertical reverse faults nucleated in shallower crustal level with vergence towards the Amazonian Craton. The third phase was less intense and shortening is accommodated in the form of fractures and subvertical sinistral faults, commonly filled by quartz veins.