CV Lattes
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Universidade Federal de São Carlos (UFSCAR). Centro de Ciências e Tecnologias para a Sustentabilidade (CCTS) (Institutional affiliation from the last research proposal) Birthplace: Brazil
graduate at Física Licenciatura from Universidade Estadual Paulista Júlio de Mesquita Filho (2005) and master's at Ciências e Tecnologia de Materiais from Faculdade de Ciências - Unesp, campus Bauru (2008). Has experience in Geosciences, focusing on Nuclear Geophysics, acting on the following subjects: traços de fissão, padrões de idade, fission track method, zircon and microestrutura. (Source: Lattes Curriculum)
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Fission Track Thermochronology (FT) has become one of the most useful techniques for reconstructing the thermal history of low-temperature rocks. In the case of sedimentary rocks, thermochronology allows for understanding evolutions of basins, as well as the regional cooling patterns of sediment source regions. The technique is based on the accumulation of tracks originating from the spon…
Despite its prominent topographic relief of up to 8 km and its location in the tropics, where erosional processes are intense, the Santa Marta Sierra Nevada (SMSN), in northern Colombia has undergone moderate uplift rates at ~0,1-0,3 mm/yr since at least 15 Ma, associated to strike-slip tectonics along the southern Caribbean Margin. This documentation has relied on bedrock and detrital th…
The tectonic evolution of the Greenstone/TTG terrain of Almas-TO is still unknown. The available U-Pb and Lu-Hf geochronological data are rare and there are no thermochronological studies by Fission-Track Thermochronology (FTT) and U-Th/He in zircon and apatite. In addition, provenance studies of the volcano-sedimentary sequences of this greenstone have not been carried out, so far. For t…
(Only some records are available in English at this moment)
The thermo-tectonic evolution of the Antarctic Peninsula is still little known. Studies in the area are being developed but with the application of techniques only within the context of geochronology that allows us to determine the age of earth materials by determining the abundance of the parent and daughter isotopes of a given isotopic system in a mineral. Using this method, such as U-P…
Zircon is a common accessory mineral in igneous, sedimentary, and metamorphic. It is physically and chemically resistant and can "survive" for many geological periods, and in many cases, it provides a record of each geological event submitted during these periods. It incorporates in its structure trace elements such as U, Th, and Pb, which is crucial for geochronological analysis. Its abi…
The thermo-tectonic evolution of the Antarctic Peninsula is still little known. Studies in the area are being developed but with the application of techniques only within the context of geochronology that allows us to determine the age of earth materials by determining the abundance of the parent and daughter isotopes of a given isotopic system in a mineral. Using this method, such as U-…
Fission Track Thermochronology (FTT) can be integrated with other methods, such as U-Pb. While the TTF preferentially provides information on low temperature events, the U-Pb registers the crystallization age of apatites (intermediate temperature events). This dual information is essential for sedimentary provenance studies (source areas) as well as the definition of geological events of …
(Only some records are available in English at this moment)
| 1 / 1 | Ongoing grants |
| 6 / 5 | Completed research grants |
| 2 / 2 | Ongoing scholarships in Brazil |
| 7 / 6 | Completed scholarships in Brazil |
| 16 / 14 | All research grants and scholarships |
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