Structural analysis is a valuable tool for organizing the stratigraphy of metamorphic terranes. It allows the reconstruction of pre-to sin-orogenic geological scenarios by unraveling the main transformations, such as distortion, rotation and translation, associated with the collisional process in orogenic belts. The BrasĂlia Orogen, for example, encompasses a complex spectrum of lithological associations and structural patterns that are not well understood because this orogenic belt still has a limited coverage of detailed structural analysis work. The implications of this are problematic for the reconstruction of pre- and sin-collisional processes related to the evolution of western Gondwana. Therefore, this contribution focuses on the Abadia dos Dourados Metavolcano-sedimentary Sequence located between the states of Minas Gerais and GoiĂĄs, Brazil. The study includes a field-based structural investigation, including geologic mapping and structural analysis at various scales of observation. It was recognized that the Abadia dos Dourados Metavolcano-sedimentary Sequence comprises a bimodal volcanic association with metarhyolite, metabasalt, banded iron formation and tourmalinite, as well as metapelites and metapsamites from base to top. The data provide additional evidence for a rift-related or back-arc basin-related model for the origin of the Meso-to Neoproterozoic volcano-sedimentary sequences in the BrasĂlia orogen. The structural framework indicates a northeast-southwest crustal shortening event associated with the collision of the Paranapanema and SĂŁo Francisco-Congo crustal blocks. The event initially produced a large (about 10 km) northeast-verging recumbent fold nappe in the area, which caused a stratigraphic inversion of the metavolcanic-sedimentary sequence. The structure underwent progressive deformation, resulting in superposition patterns between folds, foliations, and intersection lineations. In addition, the structural framework suggests that the West Gondwana collage may be related to a progressive rather than a multiphase structural evolution in the southern BrasĂlia Orogen.