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Submarine topography and faulting in Bahía de Banderas, MexicoSubmarine topography and faulting in Bahía de Banderas, Mexico
(Instituto de Geofísica, 2010)
Changing lake dynamics and sequence stratigraphy of synrift lacustrine strata in a half-graben: An example from the Triassic Ischigualasto-Villa Unión Basin, Argentina
(Wiley Blackwell Publishing, Inc, 2007-12)
Well-exposed Triassic rift strata from the Ischigualasto-Villa Unión Basin (NW Argentina) include a 80 to ca 515 m thick lacustrine-dominated package that can be correlated across a half-graben using key stratigraphic ...
The tectonic interaction between subsequent basins in the external domain of the Araçuaí Orogen: a case study of Planalto de Minas Region, Minas GeraisInteração tectônica entre bacias sucessoras no domínio externo do Orógeno Araçuaí: estudo de caso da região de Planalto de Minas, Minas Gerais
(Universidade de São Paulo, Instituto de Geociências, 2017)
Oblique half-graben inversion of the Mesozoic Neuquén Rift in the Malargüe Fold and Thrust Belt, Mendoza, Argentina: New insights from analogue models
(Pergamon-Elsevier Science Ltd, 2008-07)
The Malargüe fold and thrust belt, located in the Andean mountains between 34°S and 36°30′S, formed in response to contraction during Cenozoic times. Its structural style and geometry was controlled by the Mesozoic rift ...
Half-Graben Complex Evolution: the Rift Section of Campos Basin Based on Seismic Stratigraphic AnalysisEvolução complexa de um meio-gráben: seção rifte da Bacia de Campos baseada em análise sismoestratigráfica
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 2015)
Basement control and transfer tectonics in the Recôncavo-Tucano- Jatobá rift, Northeast Brazil
(1988)
The Reôncavo-Tucano-Jatobá rift consists of a series of asymmetric grabens which are separated by basement highs and transfer faults. Opening of the rift took place in a NW direction oblique to the N-S rift trend. Well ...
Tectonic control of the volcano-sedimentary sequence of the Chapala graben, Western Mexico
(1998)
The Chapala graben forms part of a regional system of intra-arc and half-grabens located along the western and central portions of the Mexican Volcanic Belt. Results of a stratigraphic and tectonic study of the thick, ...
Tectonic control of the volcano-sedimentary sequence of the Chapala graben, Western Mexico
(1998)
The Chapala graben forms part of a regional system of intra-arc and half-grabens located along the western and central portions of the Mexican Volcanic Belt. Results of a stratigraphic and tectonic study of the thick, ...
Arquitetura, litofácies e evolução tectono-estratigráfica da Bacia do Rio do Peixe, Nordeste do Brasil
(Universidade Federal do Rio Grande do NorteBRUFRNPrograma de Pós-Graduação em Geodinâmica e GeofísicaGeodinâmica; Geofísica, 2009-09-04)
The Rio do Peixe Basin is located in the border of Paraíba and Ceará states, immediately to the north of the Patos shear zone, encompassing an area of 1,315 km2. This is one of the main basins of eocretaceous age in Northeast ...
Synrift geometry of the Neuquén Basin in northeastern Neuquén Province, Argentina
(Geological Society of America, 2006-12)
A map of the principal grabens and half-grabens of the Neuquén Basin in the northeastern part of Neuquén Province, Argentina, was constructed based on twodimensional (2-D) and three-dimensional (3-D) seismic information. ...