CV Lattes
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Universidade Estadual Paulista (UNESP). Campus de Ourinhos. Faculdade de Ciências, Tecnologia e Educação (Institutional affiliation from the last research proposal) Birthplace: Brazil
Assistant professor at São Paulo State University (UNESP) in RDIDP, Ourinhos Campus. Graduated in Geology from São Paulo State University (UNESP), master's and doctoral degrees in Geosciences (Regional Geology) (IGCE, Rio Claro) from UNESP. Member of the CNPq research groups "Soils, Paleosols and Landscape Dynamics" - IG/Unicamp, "Soil as a record of environmental changes" Esalq-USP, and "Heritages" - Unesp. Co-organizer of DELTA H - Scientific Meeting on Landscape Evolution supported by the Serrapilheira Institute, my main research interests as a scholar are: Tectonic Geomorphology; Landscape Evolution; Cenozoic Sedimentary Basins; Hydrological Basin Dynamics and Reorganization; Landslides and River Captures; Quaternary Studies; Quantitative Geomorphology; Geodiversity, Geoconservation, Geotourism, Geoeducation, and Natural Heritage. I collaborate as a research associate on projects with ESALQ - USP (Graduate Program in Soil Science and Plant Nutrition), UFPR (Graduate Program in Geology), CUNY (USA), and IG-UNICAMP. I have 9 years of experience in managing a Public Higher Education Institution and have served as an "ad hoc" evaluator for over 20 years for the São Paulo State Education Council. I have also served as the Coordinator of the Geography (Bachelors and Teaching Degree) program at Unesp, Ourinhos Campus, from November 2022 to September 2024. (Source: Lattes Curriculum)
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The relationship between the relief evolution, sedimentation and tectonic activity, either in active margin or in intraplate area, is growing in importance among researchers specialized in studies of the Cenozoic. With respect to the das Cinzas watershed, such integrated studies considering the relationship between morphogenesis, sedimentation and neotectonic are nonexistent. Thus, this p…
After a century-long process of sequential hydroelectric plant installations along its course, the Paranapanema River now retains only seven kilometers of its original channel, located in the Tourist Municipality of Piraju (SP). The remaining rapids, characteristic of a bedrock river, cut through trachydacites and volcanic features associated with the Paraná-Etendeka Igneous Province-uniq…
This project is part of a larger project toward a better understanding of sedimentation, morphogenesis, and Cenozoic tectonics of the das Cinzas river hydrographic basin, northern Paraná. The objectives consist of outlining the morphostructural framework of the area covered by the IBGE topographic sheets "Santo Antonio da Platina" and "Ribeirão do Pinhal" on a scale of 1:50.000 (sheets SF…
This project is part of a larger project toward a better understanding of sedimentation, morphogenesis, and Cenozoic tectonics of the das Cinzas river hydrographic basin, northern Paraná. The proposed objectives relate to the identification, mapping at 1:50,000 scale, and morphological characterization of occurrences of Quaternary deposits in the das Cinzas river hydrographic basin (north…
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