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Metamorphic, partial melting and deformation studies in high-pressure metapelitic rocks

Grant number: 15/05230-0
Support type:Regular Research Grants
Duration: October 01, 2015 - December 31, 2017
Field of knowledge:Physical Sciences and Mathematics - Geosciences
Principal Investigator:George Luiz Luvizotto
Grantee:George Luiz Luvizotto
Home Institution: Instituto de Geociências e Ciências Exatas (IGCE). Universidade Estadual Paulista (UNESP). Campus de Rio Claro. Rio Claro , SP, Brazil
Assoc. researchers: Andreas Kronz ; Caio Arthur Santos ; Daniel Francoso de Godoy ; Edson Ricardo Maia Ferraz ; Luiz Sérgio Amarante Simões ; Rafael Vieira Ribeiro ; Regiane Andrade Fumes ; Renato de Moraes ; Thomas Zack

Abstract

The present work focuses on the metamorphic characterization of high pressure metapelitic rocks from two localities in Southern Minas Gerais State. The study rocks record metamorphic processes and deformation that took place in the Neoproterozoic, during the Brasiliano Orogeny. They belong to the Brasilia Belt (Passos / São Sebastião do Paraíso Region - SSP) and Ribeira Belt (Luminárias Region - LM). Rocks from SSP have the mineral assemblage Grt+KFs+Ky+Rt and show abundant layers of KFs+Qtz, indicating partial melting at high-pressure granulite facies (corroborated by retroeclogite occurrences). Phylites and schists from LM fall in the field of high Al pelites. These rocks show mineral assemblages that differ from those of pelites from the classic barrovian series, since Bt is not crystalized under greenschist and amphibolite facies. Highest grade rocks from LM have the mineral assemblage Grt+St+Ky, which is indicative ob amphibolite facies (Ky zone). Metamorphic studies have previously been carried out in both areas. However, they did not include modern techniques like, pseudosection, and trace-element geothermobarometers, such as Zr-in-Rutile and Ti-in-Quartz. The aim of the present study is to calculate peak P-T conditions for these rocks, as well as U-Th-PbT monazite ages. Together with petrographic and field observation, the data will be used to construct P-T-t-d paths for the study rocks. The new data will favor discussion about the interference zone between Brasilia and Ribeira belts, shedding light into the formation of southern São Francisco Craton region. The project also aims to develop and implement trace element analyses in the EPMA laboratory at Unesp - Rio Claro, where it has recently been installed a JEOL JXA 8230. Protocols will include trace element analyses in Rt (V, Cr, Fe, Zr, Nb, Sn, Sb, Hf, Ta, e W), Ti in Qtz, as well as U-Th-PbT monazite dating. (AU)

Scientific publications
(References retrieved automatically from Web of Science and SciELO through information on FAPESP grants and their corresponding numbers as mentioned in the publications by the authors)
REGIANE ANDRADE FUMES; GEORGE LUIZ LUVIZOTTO; RENATO MORAES; MONICA HEILBRON; SILVIO ROBERTO FARIAS VLACH. Metamorphic modeling and petrochronology of metapelitic rocks from the Luminarias Nappe, southern Brasilia belt (SE Brazil). BRAZILIAN JOURNAL OF GEOLOGY, v. 49, n. 2, p. -, 2019. Web of Science Citations: 0.

Please report errors in scientific publications list by writing to: cdi@fapesp.br.