CV Lattes
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Universidade de São Paulo (USP). Instituto de Geociências (IGC) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Bachelor's degree in Geology from the University of São Paulo (2008). Master's (2011) and PhD (2015) in the Mineralogy and Petrology Program at the Institute of Geosciences, University of São Paulo (IGc-USP). Internship (BEPE-FAPESP) at the School of Earth and Environmental Sciences, University of St Andrews (Scotland) in 2014. Conducted postdoctoral research from 2016 to 2019 in the Geochemistry and Geotectonic Program at IGc-USP and from 2020 to 2024 in the Mineralogy and Petrology Program at IGc-USP. Currently developing a postdoctoral project in the Department of Mineralogy and Geotectonics aiming to establish a highly reliable methodology for predicting the emplacement mode of volcanic rocks to assist in the paleoenvironmental reconstruction of volcano-sedimentary sequences. Research interests: elemental and isotopic geochemistry (bulk rock and mineral), geochronology, thermochronology, petrochronology, and quantitative textural analysis (CSD + EBSD), applied to petrology and crustal evolution studies. (Source: Lattes Curriculum)
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Thermochronology is a technique that applies chemical and isotopic systems in order to extract evidences on the thermal history of rocks, minerals and geological terranes. The comprehension of the thermal history, allied to other geological information, allows the establishment of the period/age of geological processes. This knowledge is essential to the understanding of Earth's evolution…
The southern margin of the Brasília Orogen is characterized by an ediacaran nappe system formed during the collision between the São Francisco and Paranapanema paleocontinentes. In this nappe system the superior alocthons were laterally transported to the southern margin of the São Francisco Craton (Socorro-Guaxupé Nappe and Andrelandia Nappe System), while the inferior alocthons were tra…
Zircon is the most used mineral in studies of metasedimentary rocks provenance because of its resistance to intemperism, diagenesis and metamorphism. Nowadays, studies of the U-Pb and Lu-Hf isotopic system are the main tools used in such studies, because the first separates crystal populations by age and the second yields information about crustal and mantle contributions.Prof. Dr. Hawkes…
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