Existing models of tectonic evolution of the Neoproterozoic orogenic system rimming the shores of the South Atlantic Ocean (the Araçuaí–Ribeira–Congo and Dom Feliciano–Kaoko …
Abstract Field, petrographic, geophysical, geochronological, elemental and isotopic data support the identification of distinct components of a Wilson cycle (rift-drift-subduction …
The Araçuaí belts extends along the curved southeastern margin of the São Francisco craton between the Brazilian coast and Lat 21° S, where it merges with the Ribeira belt. It …
Gondwana was consolidated in the late Cambrian after 180 myr of tectonic convergence among Neoproterozoic paleocontinents and smaller fragments. We present a compilation of …
The Araçuaí orogen and West Congo belt make up a singular confined orogenic system, embraced by the San Francisco–Congo craton: the AWCO. It includes a southern sector with …
Abstract The Neoproterozoic Araçuaí-West Congo orogen in Brazil and Congo represents a branch of the Brasiliano/Pan-African orogenic system that is considered to terminate …
Abstract The Tonian Serra da Prata magmatic arc is part of an association of several magmatic arcs of the Ribeira orogenic system in Southeastern Brazil. Along with the …
Understanding the evolution of the Chotanagpur Granite Gneiss Complex (CGGC) of the East Indian Shield is crucial to decipher the role of the Indian Shield in the formation of the …
R Degler, A Pedrosa-Soares, I Dussin, G Queiroga… - Gondwana …, 2017 - Elsevier
The Araçuaí orogen and the Ribeira belt make up a complex Neoproterozoic-Cambrian orogenic system, the Araçuaí-Ribeira orogenic system (AROS) located from the eastern to …