CV Lattes
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Universidade Estadual Paulista (UNESP). Campus de Rio Claro. Instituto de Geociências e Ciências Exatas (IGCE) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Geologist graduated from São Paulo State University (UNESP), with an emphasis on structural geology, fracturing pattern and mechanical stratigraphy. Master degree in Geosciences and Environment from São Paulo State University (UNESP), working with structural geology and relationships with slope and slope stability, landslides, and debris flows. PhD degree in Geoscience and Environment at the São Paulo State University (UNESP), working with stratigraphy, sedimentology, geochronology and sedimentary provenance. My research currently involves applying geochronology and isotope geochemistry to solve and understand a diverse series of questions about sedimentary basins evolution, geodynamics, and crustal evolution . It is based mainly around: (i) The application of laser-ablation ICP-MS techniques to isotopic dating of sedimentary deposits and sedimentary provenance analysis; (ii) The use of Electron Probe Microanalyzer (EPMA) techniques to geochemical analysis of accessory minerals; (iii) Characterization of minerals using Scanning Electron Microscopy (SEM); (iv) Integrated analysis between sedimentological and stratigraphical analysis and geochronological and provenance data; (v) Geodynamics, plate tectonics, and crustal evolution. (Source: Lattes Curriculum)
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The earth is the only planet in the Solar System that is characterized by an active plate tectonic regime, that is responsible for cyclic supercontinent formation and played a major role in the atmosphere oxygenation, the addition of nutrients to the ocean and produced resources that supported the biosphere. There is still no consensus about the age that plate tectonics was fully operatio…
The Andrelândia Group (Neoproterozoic) is situated in the Brasília Orogen in the southern border of São Francisco Craton, being composed of two depositional sequences and four lithostratigraphic units. The Andrelândia Group succession consists of a nappe system (Andrelândia Nappe System), which developed fold-and-thrust belt structures due to the convergence between the Brasília and Ribei…
The Cariri and Tacaratu formations are part of the Paleozoic basal units of the Araripe and Jatobá/Tucano Norte, and are historically interpreted as distant correlates of the Ipu Formation sediments (Parnaíba Basin). The Paleozoic lower units of the Brazilian cratonic basins are very important to understand and interpret initial sedimentation ages, paleogeography and depositional styles d…
(Only some records are available in English at this moment)
The Andrelândia Group is located on the southern border of the São Francisco Craton and is situated in an interference zone between the Brasília and Ribeira Orogen, characterized by the presence of folds and thrusts. The group was formed from the collision between the Paranapanema and São Francisco Cratons in the Brasiliano Orogeny (Neoproterozoic). The Andrelândia Group is composed of tw…
The Cariri and Tacaratu formations are part of the Early Paleozoic basal units of the Araripe and Jatobá/Tucano Norte, and are historically interpreted as distant correlates of the Ipu Formation sediments (Parnaíba Basin). The Paleozoic lower units of the Brazilian cratonic basins are key units to understand and interpret initial sedimentation ages, paleogeography and depositional styles …
The origin of intracratonic basins is currently one of the most prolific topics in the geologic sciences, constituting a challenge in itself. The complexity of this theme, added to the necessity of an integrated approach based in a multi-proxy analysis, places this study on the frontier of modern science. The almost complete lack of integrative studies focused in sedimentological, stratig…
| 1 / 1 | Ongoing grants |
| 5 / 5 | Completed scholarships in Brazil |
| 3 / 3 | Completed scholarships abroad |
| 9 / 9 | All research grants and scholarships |
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