Currently, she is a PhD Student in Earth Sciences at the University of Toronto (UofT), in Canada. She graduated in Geology in 2017 from the University of São Paulo (USP) where she also concluded her MSc in Metamorphic Petrology. During her period at the USP, she developed research working with the metamorphism of metapelites on the Ribeira Belt. The project combined techniques such as thermodynamic modelling, petrochronology, and detrital zircon provenance to better understand the tectonic evolution of the area. She also did an internship during her MSc at the University of Portsmouth, UK where she worked with in situ monazite dating with LA-ICP-MS. All her research in Brazil was financed by the São Paulo State Research Foundation. In her PhD, she develops research aiming to better understand the entrapment of melt inclusions in olivine through experimental petrology, stable isotope geochemistry and modelling. She also has experience with field geology and geological mapping, being a teacher assistant on mapping courses at both USP and UofT. (Source: Lattes Curriculum)
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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 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…
| 2 / 2 | Completed scholarships in Brazil |
| 1 / 1 | Completed scholarships abroad |
| 3 / 3 | All Scholarships |
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