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Estruturas rúpteis e expressão topográfica na terminação norte da Serra da Mantiqueira, Sudeste do Brasil
(Universidade Federal de Minas GeraisBrasilIGC - INSTITUTO DE GEOCIENCIASPrograma de Pós-Graduação em GeologiaUFMG, 2021-06-16)
Elevated Passive Continental Margins (EPCMs) are characterized by extensive topographic elevations, such as sharp escarpments, located at the transition between a low-relief elevated inland plateau and narrow coastal plains. ...
Dating recurrent shear zone activity and the transition from ductile to brittle deformation: white mica geochronology applied to the neoproterozoic Don Feliciano Belt in South Brazil
(Pergamon-Elsevier Science Ltd, 2020-09-22)
Argon geochronology of white mica has a good potential of recording recurrent dynamic recrystallization in shear zones in the transition from ductile to brittle deformation, as temperature ranges for mineral crystallization ...
Size effects in the transition region and the beginning of the upper shelf for ferritic steels
(Wiley Blackwell Publishing, Inc, 2010-02-03)
The determination of a characteristic fracture toughness value for ferritic steels in the ductile-to-brittle transition regime becomes difficult due to the scatter observed in the results. As the temperature increases, ...
BRITTLE TECTONICS OF THE REGION BETWEEN PILAR DO SUL AND VOTORANTIM, SPTECTÔNICA RÚPTIL DA REGIÃO ENTRE PILAR DO SUL E VOTORANTIM, SP
(Sociedade Brasileira de Geologia, 2017)
BRITTLE STRUCTURAL ANALYSIS IN THE INFLUENCE ZONE OF THE PONTA GROSSA ARCH: CASE STUDY IN THE AREA OF THE HPP-MAUÁ-PRANÁLISE ESTRUTURAL RÚPTIL NA ZONA DE INFLUÊNCIA DO ARCO DE PONTA GROSSA: ESTUDO DE CASO NA ÁREA DA UHE-MAUÁ-PR
(Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista, 2020)
Sistemas orbitais e aéreos aplicados à análise multi-escala da tectônica rúptil atuante na borda sudeste da Bacia do Parnaíba
(Universidade Federal do Rio Grande do NorteBRUFRNPrograma de Pós-Graduação em Geodinâmica e GeofísicaGeodinâmica; Geofísica, 2006-08-25)
The tectonics activity on the southern border of Parnaíba Basin resulted in a wide range of brittle structures that affect siliciclastic sedimentary rocks. This tectonic activity and related faults, joints, and folds are ...