Metamorphic pressure–temperature (P–T) conditions in the Southern Brasília Orogen are relatively well constrained, particularly in its southernmost segments. However, the central and northern portions need further attention, especially regarding the metamorphism affecting the volcano-sedimentary sequences of the Arenópolis Magmatic Arc (AMA). The Anicuns–Itaberaí Sequence (AIS), located in the southern segment of the AMA, comprises a well-exposed metavolcano-sedimentary succession of mafic to ultramafic metavolcanic rocks, metachert, metarhythmite, marble lenses and quartzite. Well-preserved outcrops in the lowlands surrounding the Serra da Jiboia region, located in the central portion of the study area, were used to investigate the structural features and deformation recorded in metasedimentary rocks of the AIS and two samples of metagreywackes were selected for metamorphic modelling. The analyzed rocks correspond to garnet–chlorite–biotite–muscovite schists and were selected for microstructural analysis, quantitative mineral mapping, and thermodynamic modelling based on electron microprobe analyses. The results indicate that the peak metamorphic assemblage (garnet + biotite + plagioclase + muscovite + rutile +ilmenite) was stable at temperatures above 600 °C and pressures exceeding 0.95 GPa. The metamorphic evolution, inferred from compositional zoning in garnet, defines a clockwise P–T path, with initial garnet growth at 525–555 °C and 0.67–0.77 GPa, a metamorphic peak at 660 °C and 1.16-1.30 GPa, followed by decompression between 550 to 585 °C and 0.65-0.79 GPa. These results indicate that the AIS schists reached high-pressure amphibolite-facies conditions, exceeding those typical of the Barrovian metamorphism, and point to a collisional tectonic regime characterized by deep crustal burial and subsequent exhumation. Deformation structures were chronologically classified into four distinct phases (D 1 to D 4 ). The main deformation event (D 2 ) is characterized by asymmetric folding, while subsequent reverse faulting and shearing (D 3 ) are associated with post-burial exhumation during syn-collisional processes. Microstructural evidence suggests that the metamorphic peak likely occurred between the end of D 1 and the onset of D 2 , indicating that peak mineral growth was broadly synchronous with early stages of the main deformation phase and burial. • Garnet core began to crystallize mid D 1 -D 2 stages at 525-550 °C and 0.67-0.77 GPa • Metamorphic peak at 660 °C and 1.16-1.3 GPa; decompression at 550 °C and 0.65 GPa • Stability conditions of the paragenesis indicate metagreywackes protolith • Four stages of deformation, from crustal thickening to structural stabilization
Passo-Vieira et al. (Fri,) studied this question.