dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T11:20:21Z
dc.date.available2014-05-27T11:20:21Z
dc.date.created2014-05-27T11:20:21Z
dc.date.issued2001-12-01
dc.identifierRevista Brasileira de Geofisica, v. 19, n. 2, p. 131-144, 2001.
dc.identifier0102-261X
dc.identifierhttp://hdl.handle.net/11449/66689
dc.identifier10.1590/S0102-261X2001000200002
dc.identifierS0102-261X2001000200002
dc.identifier2-s2.0-30544439550
dc.identifier2-s2.0-30544439550.pdf
dc.identifier1989662459244838
dc.description.abstractThis paper presents the gravity survey refinement of the Paraíba do Sul river valley, east region of São Paulo state, by acquisition of 646 gravity stations. Further than the traditional Free-Air and Bouguer corrections, it was necessary to apply the Terrain Correction due the proximity of the Mantiqueira and Mar mountain ranges. An enhanced understanding of Taubaté Basin structural framework was the main objetive of this work. As result, we present the Bouguer Gravity Map of the east region of São Paulo State and the Residual Bouguer Gravity Map generated by Upward Continuation and High-pass filtering. The 2D Gravity Modeling was applied in 4 sections, using bi-dimensional models for the bodies that produced the anomalies (Talwani Method). After integrating the gravity data with the interpretation of 11 seismic sections, it was possible to delineate the Taubate Basin structural framework, which shows an utmost sedimentary thickness of 800 m in the depocenters. It was also interpreted an ultramaphic alkaline plug in the subsurface of Caçapava city.
dc.languagepor
dc.relationRevista Brasileira de Geofísica
dc.rightsAcesso aberto
dc.sourceScopus
dc.subjectBouguer Gravity Map
dc.subjectGravity
dc.subjectModeling
dc.subjectTaubaté Basin
dc.subjectBouguer anomaly
dc.subjectgravity survey
dc.subjectBrazil
dc.subjectSao Paulo [Brazil]
dc.subjectSouth America
dc.titleModelagem gravimétrica da Bacia de Taubaté-vale do Rio Paraíba do Sul, leste do estado de São Paulo
dc.typeArtículos de revistas


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