Análise estrutural da tectônica deformadora da Bacia de Itajaí, estado de Santa Catarina, Brasil.
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1992
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Abstract
Structural analysis of the Itaja" Group has confirmed and increase in deformation magnitude
from NW to SE, toward the more deformed zone of the Dom Feliciano mobile belt. This condition is in
agreement with the predicted characteristics of a foreland basin deformed in a convergent environment. Two
families of tectonic structures were recognized, both corresponding to different deformation phases and
associated stress fields. The first represents the late collisional phase of the orogenic cycJe, which caused the
development of reverse faults, asymmetric folds, and a conjuga te system of strike-slip faults. The progressive
evolution of this convergence led to the change from a frontal to an oblique collision, with dextral-reverse
kinematics. The second phase records a post-collisional extensional pulse, leading to the reactivation of earlier
structures and inversion of movements along the conjugate system of strike-slip faults.
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Citation
ROSTIROLLA, S. P.; SOARES, P. C.; ALKMIM, F. F. de. Análise estrutural da tectônica deformadora da Bacia de Itajaí, estado de Santa Catarina, Brasil. Boletim de Geociências da Petrobrás, Rio de Janeiro, v. 6, n. 3/4, p. 123-147, 1992. Disponível em: <http://publicacoes.petrobras.com.br/main.jsp?lumPageId=8A9E308F545405DE0154A04B46AD0C9E&lumItemId=8A9D2AAF5BFE776F015C3687D3585AFB&previewItemId=8A9D2AAF5BFE776F015C3687D34F5AFA&publicacaoId=8A9D2AAF5A284744015A2958DE4D3BC9#>. Acesso em: 20 jun. 2017.