CV Lattes
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Universidade de São Paulo (USP). Instituto de Geociências (IGC) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Ginaldo A. da C. Campanha is Geologist and Senior Professor of the Institute of Geosciences of University of São Paulo. He got his PhD on Geotectonics at the same university in 1992. His main research interests have been in Tectonics, Structural Geology and Regional Geology of the Southeast Brazil. (Source: Lattes Curriculum)
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The main scope of this proposal is to compare Phanerozoic fold-and-thrust belts with their Proterozoic equivalents in terms of their deformational styles and regimes. The study will be carried out through the construction of geological cross-sections orthogonal to the structures, geometrically controlled, balanced and restorable, based on field surveys, existing geological cartography and…
The San Francisco Craton is delimited by marginal fold-and-thrust belts which affect its Paleo, Meso and Neoproterozoic covers, and in the neighboring orogens also involve its basement. In its southeastern portion is circumscribed by the Araçuaí Belt, whose most adopted craton boundary corresponds to the thrust front that pulls the Espinhaço Supergroup over the Neoproterozoic cover of the…
(Only some records are available in English at this moment)
The southern Ribeira Belt is the result of an oblique collision between the São Francisco,Paranapanema and Luís Alves cratons, with the participation of microplates andallochthonous terrains remobilized during the Brasiliano-Pan-African cycle. This processresulted in a series of juxtaposed domains limited by shear zones that accumulatedappreciable horizontal displacements, some of which c…
The Paramirim aulacogen is understood as an intracontinental rift system, nucleated around 1.75 Ga, in the central region of the São Francisco craton (SFC), which allowed the deposition of thick sedimentary sequences, predominantly siliciclastic and carbonate, such as the Espinhaço and São Francisco supergroups. The complex tectonic evolution of the CSF ultimately involved an intense proc…
The aim of this project is to analyze the deformation of the Espinhaço Supergroup in the western portion of Chapada Diamantina, Bahia, by the construction and restoration of balanced geological cross sections, and the analysis of the finite deformation suffered by the rocks. These objectives will be achieved by applying geometric techniques in the construction of cross sections and verifi…
(Only some records are available in English at this moment)
Understanding the kinematics and deformation timing of ductile shear zones is essential for reconstructing the temporal evolution of metamorphic terranes and contributes significantly to tectonic models of continental assembly. Accurately constraining the time evolution of shear zones remains challenging due to the difficulty of determining the exact timing of ductile deformation (mylonit…
The development of the Ribeira Belt, SE Brazil, is dominated by shear zone system established between Ediacarano and Cambrian and characterized by brittle-ductile to ductile shear zones. The Taxaquara Shear Zone (TSZ) was one of the first transcurrent structures of regional relevance identified in the Ribeira Belt, having been attributed to it great importance in the tectonic compartmenta…
The Taxaquara Shear Zone was one of the first regional transcurrent structures of importance identified in the Ribeira Belt, having been assigned to it great importance in the tectonic subdivision of the Belt. Despite the importance that has been attributed to it, the Taxaquara Shear Zone has been very little addressed in specific studies since its original definition for nearly half a ce…
| 1 / 1 | Ongoing grants |
| 17 / 7 | Completed research grants |
| 10 / 6 | Completed scholarships in Brazil |
| 1 / 1 | Ongoing scholarships abroad |
| 2 / 2 | Completed scholarships abroad |
| 31 / 17 | All research grants and scholarships |
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