Using elastic geobarometry to unveil subduction-collision and rapid exhumation in the West Gondwana Orogen: Application to high-T/HP rocks in the NW part of the Borborema Province, NE Brazil

Autor(es)

Aires, Felipe da Silva ; dos Santos, Lucilene ; de Moraes, Renato ; de Oliveira, Armando Lucas Souza ; Gilio, Mattia ; Pestilho, Andre Luiz Silva ; dos Santos, Felipe Holanda ; Cruz, Carlos Eduardo Maciel

• Tipo de documento: Artigo Científico
• Fonte: LITHOS; v. 494, p. 11-pg., 2024-12-21.

Resumo

Elastic geothermobarometry is a method used to estimate pressure and temperature (P-T) conditions based on the residual pressure exhibited by mineral inclusions entrapped in a host. In this study, we present micro-Raman spectroscopic data for quartz inclusions in host garnet from a retrograde mafic granulite and a retrograded eclogite from the Carire<acute accent> Granulite Zone and Forquilha Eclogite Zone, Ceara<acute accent> Central Domain, northwestern Borborema Province, northeastern Brazil. Elastic modeling using the Quartz-in-Garnet geobarometer suggests residual pressure (Pinc) values between -0.14(6) and - 0.01(6) GPa for the mafic granulite, and a range of 0.06 (6) to 0.54(4) GPa for the eclogite, indicating that some inclusions are under tensile stresses (i.e., negative Pinc) while other experienced compressive stresses (i.e., positive Pinc). Isomekes built using Equations of State (EoS) for almandine garnet yield an entrapment pressure (Ptrap) value of 1.35(2) GPa at 910 degrees C for the retrograde mafic granulite, whereas retrograded eclogite isomekes indicate a Ptrap value of 1.68(6) GPa at 770 degrees C. These findings suggest that the volumetric response of quartz inclusions to pressure and temperature changes during exhumation to Earth's surface resulted in compressive and tensile stresses, consistent with the pressure conditions for the Forquilha and Carire<acute accent> zones, as determined by conventional geothermobarometry. Compressive and tensile stresses result from decompression within the stability field of alpha-quartz. Retrograded eclogite entrapment pressure (Ptrap) of 1.68(6) GPa suggests metamorphism at the base of a thickened continental crust (ca. 61 km). In contrast, the retrograde mafic granulite pressure of 1.35(2) GPa indicates peak metamorphic conditions during the collisional stage at a burial depth of ca. 49 km. The observed variability in residual pressures suggests a relatively fast exhumation for this segment of the West Gondwana Orogen. (AU)

• Processo FAPESP: 23/17675-2 - Datando processos deformacionais na crosta continental média a superior: uma investigação geocronológica multimétodo no Orógeno Brasília Meridional
• Beneficiário: Armando Lucas Souza de Oliveira
• Modalidade de apoio: Bolsas no Brasil - Doutorado
• Processo FAPESP: 23/07347-8 - Metamorfismo e fusão parcial em orógenos antigos III
• Beneficiário: Renato de Moraes
• Modalidade de apoio: Auxílio à Pesquisa - Regular