graduation at Geologia from Universidade Estadual Paulista Júlio de Mesquita Filho (1988), master's at Geology from Universidade de Brasília (1992) and doctorate at Geology from Universidade de Brasília (1997). Has experience in Geosciences, focusing on Petrology, acting on the following subjects: granulito, migmatito, metamorfismo, ultra high temperature metamorphism and fusão. I do frequent reviews for : Journal of Metamorphic Geology, Lithos, Precambrian Research, Journal of Petrology, International Journal of Earth Sciences, Journal of South America Earth Sciences, Brazilian Journal of Geology, Revista Geologia USP, Geociências UNESP and sporadic ones for other journals (e.g. Tectonophysics, Chemical Geology, European Journal of Mineralogy, Gondwana Research, GSA Memoir, European Journal of Geology). Consultor ad hoc for FAPESP. CNPq Researcher - Level 2 (Source: Lattes Curriculum)
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The raising of mountain belts is a consequence of tectonic activity and the collision of plates, and the highest mountains are formed when two continental plates collide. The Continental geotherm is doubled and the accumulated heat generates metamorphism and partial melting, which transform and differentiates the continental crust, an irreversible process that is registered in the formed …
This research project aims to investigate the tectonic evolution of ancient orogens using the study of metamorphic rocks. Metamorphism and partial melting are direct consequences of the thermal relaxation following the collisional stage in orogens. The shape of the P-T paths, the partial melting reactions and formed parageneses are reflections of tectonic history that the rock underwent, …
This research project aims to investigate the the tectonic evolution of ancient orogens through the study of metamorphic rocks. Metamorphism and partial melting are direct consequences of the thermal relaxation that follows the collisional stage in orogens. The shape of the P-T paths, melting reactions and mineral paragenesis are reflexes of the tectonic history the rock underwent, so the…
The formation of Antarctic Peninsula is related to Gondwana break-up. The rocks that compose the peninsula are related to a fore-arc basin, island arc and a back arc basin system, which was installed in a continental crust in the Gondwana pacific coast, between Triassic and Jurassic. The turbiditic sediments were deposited in an accretionary prism and are now represent by the rocks of the…
(Only some records are available in English at this moment)
Metatexites are rocks that underwent partial melting but still had a part of their original structure, such as stratification and foliation, preserved. During tectonic processes of collisional interaction between the San franciscana and Paranapanemaplates, in the Neoproterozoic, a variety of metamorphic and deformed rocks were generated, among them, the metatext. These occupy different te…
In the Ribeira Belt, between the States of São Paulo and Paraná, Brazil, metasedimentary rocks from Turvo-Cajati Formation crop out. There are some recent studies that point to distinct metamorphic field gradients in the same unit. The baric regime in partially molten granulite facies rocks indicates pressure above 9 kbar (Faleiros, 2008), whereas amphibolite facies rocks record a barrovi…
In the region of Vale do Ribeira, in the states of São Paulo and Paraná, crop out metamorphic rocks with different conditions of temperature and pressure. Rocks of lower green schist facies, amphibolite facies and even rocks with evidences of partial melting can be found, and these are related to Turvo-Cajati Formation. The prior characterization of the metamorphism in these rocks points …
In the Southern Brasília Orogen occurs associations of metamorphic rocks, which were formed during the closure of Gondwana, in the Neoproterozoic. Between them, the Soccoro-Guaxupé Nappe, an allochton terrane, was exposed to extreme metamorphic conditions, reaching conditions of ultra-high temperature, above 900 °C. Besides granulites, there are migmatites, with variable rate of partial m…
(Only some records are available in English at this moment)
Thermodynamic modeling is an important tool for investigating and quantifying the metamorphic processes that occurred during history of Earth. It is through it that thermobarometric results are obtained and mineral stability relationships are calculated (Lanari & Hermann, 2020). Due to the progress of technologies in the 21st century, a big advance occurred in the field of computational p…
In Ribeira Belt, SE Brazil, metasedimentary rocks of distinct pressure conditions crop out. However, they are all assumed to be part of the same unit, the Turvo-Cajati Formation (TCF). A better understanding in P-T-t paths in this unit could help have a better picture of the conditions that lead to their current disposition. TCF is a metasedimentary unit forming the Curitiba Terrane, a ma…
Timescales, over which high-grade metamorphism occurs, are required in order to fully integrate petrological data into tectonic frameworks. In the absence of geochronological constraints, the shape of a P-T path does not necessarily indicate the tectonic setting of metamorphism. Zircon, monazite and titanite are common accessory phases in many rock types, including the ones underwent high…
(Only some records are available in English at this moment)
| 1 / 1 | Ongoing research grants |
| 5 / 4 | Completed research grants |
| 1 / 1 | Ongoing scholarships in Brazil |
| 14 / 11 | Completed scholarships in Brazil |
| 5 / 4 | Completed scholarships abroad |
| 26 / 21 | All research grants and scholarships |
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CV Lattes
ORCID