A5026627318- Geological formations and processes
- Geological and Geophysical Studies
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- Geography and Environmental Studies
- Hydrocarbon exploration and reservoir analysis
- Geological Modeling and Analysis
- Hydraulic Fracturing and Reservoir Analysis
- Reservoir Engineering and Simulation Methods
- Fish biology, ecology, and behavior
- Oil Spill Detection and Mitigation
- Maritime and Coastal Archaeology
- Seismic Imaging and Inversion Techniques
- Geological Studies and Exploration
- Geology and Paleoclimatology Research
- Paleontology and Stratigraphy of Fossils
- Geophysical and Geoelectrical Methods
Universidade Federal do Rio de Janeiro
2024
Petrobras (Brazil)
1988-2017
Research Article| May 01, 2012 Episodic burial and exhumation in NE Brazil after opening of the South Atlantic Peter Japsen; Japsen † 1Geological Survey Denmark Greenland (GEUS), Øster Voldgade 10, 1350 Copenhagen, †E-mail: pj@geus.dk Search for other works by this author on: GSW Google Scholar Johan M. Bonow; Bonow Paul F. Green; Green 2Geotrack International, 37 Melville Road, Brunswick West, Victoria 3055, Australia R. Cobbold; Cobbold 3Géosciences (UMR6118), Centre National de la...
The Recôncavo‐Tucano‐Jatobá (RTJ) Rift and many other smaller sedimentary basins in northeast Brazil formed during South Atlantic rifting were subsequently uplifted exhumed so that Albian marine sediments are now located up to 800 m above sea level some 400 km inland from the margin. Local erosion caused by footwall uplift regional erosion, probably resulting magmatic underplating uplift, has removed a large part of thermal sag phase RTJ Rift. flexural cantilever model, incorporating...
Release faults are rift cross faults, which develop to accommodate the variable displacements of hanging-wall block along strike normal faults. nearly perpendicular or obliquely oriented fault they related to. They have maximum throws adjacent parent and die out in hanging wall away from it. form release bending stresses do not reflect orientation regional stress field a basin. Commonly, show normal-oblique preferentially located ramps. may also act at scale an entire basin, reaching...
We investigate the crustal architecture and structural domains of Campos rifted margin in southeastern Brazil, focusing on rifting evolution segmentation. Based 2-D 3-D seismic reflection interpretation potential field modelling, our results reveal an along-strike variability, terms magmatism, that segments basin into three main sectors from south to north. Through analysis profiles, we interpret this lateral variability as a product lower- upper-plate alternations different magmatic inputs....
Until recently, the Lower Cretaceous Recôncavo-Tucano-Jatobá Rift was interpreted as being a system of basins connected since beginning rifting and filled by fluvio-deltaic-lacustrine which prograded from north to south. In this work, based on field observations, gravity data, new models for evolution continental rifts, comparison with East African are series half-grabens disconnected depocenters, evolved separately. The isolation effected transfer faults - Itapicuru Vaza-Barris cut rift in...
We investigate the crustal architecture and structural domains of Campos rifted margin in southeastern Brazil, focusing on rifting evolution segmentation. Based 2-D 3-D seismic reflection interpretation potential field modelling, our results reveal an along-strike variability, terms magmatism, that segments basin into three main sectors from south to north. Through analysis profiles, we interpret this lateral variability as a product lower- upper-plate alternations different magmatic inputs....
Abstract We investigate the crustal architecture and structural domains of Campos rifted margin in southeastern Brazil, focusing on rifting evolution segmentation. Based 2‐D 3‐D seismic reflection interpretation potential field modeling, our results reveal an along‐strike variability, terms magmatism, that segments basin into three main sectors from south to north. Through analysis profiles, we interpret this lateral variability as a product lower‐ upper‐plate alternations different magmatic...
Download This Paper Open PDF in Browser Add to My Library Share: Permalink Using these links will ensure access this page indefinitely Copy URL The Espadarte Transfer Zone: Structural Architecture and Kinematics of an Oblique Basement High Controlling Pre-Salt Geometry Campos Basin, Se Brazil 41 Pages Posted: 23 Feb 2024 See all articles by Debora Lopes Pilotto DominguesDebora DominguesFederal University Rio de JaneiroRenata ZanellaFederal JaneiroLuciano Magnavitaaffiliation not provided...
Until recently, the Lower Cretaceous Recôncavo-Tucano-Jatobá Rift was interpreted as being a system of basins connected since beginning rifting and filled by fluvio-deltaic-lacustrine which prograded from north to south. In this work, based on field observations, gravity data, new models for evolution continental rifts, comparison with East African are series half-grabens disconnected depocenters, evolved separately. The isolation effected transfer faults - Itapicuru Vaza-Barris cut rift in...