Gondwanaland lasted from the 650–500 Ma (late Neoproterozoic-Cambrian) amalgamation
of African and South American terranes to Antarctica–Australia–India through 320 Ma (mid …

This synthesis presents the complex evolution of two different magmatic arc systems in the
Ribeira belt, which were progressively accreted onto the southeastern and southern border …

The history of the geologic evolution of the South American continent from the
Neoproterozoic to the early Cambrian is recording all the steps of the development of a …

The Dom Feliciano Belt is an important Neoproterozoic to Cambrian orogenic complex,
extending from eastern Uruguay to southern Brazil. It comprises a collage of oceanic …

Abstract Field, petrographic, geophysical, geochronological, elemental and isotopic data
support the identification of distinct components of a Wilson cycle (rift-drift-subduction …

Palaeomagnetic apparent polar wander (APW) paths from the world's cratons at 1300–700
Ma can constrain the palaeogeographic possibilities for a long-lived and all-inclusive …

The Mantiqueira Province (MPV) is a large, complex structural province deformed by the
Neoproterozoic/Early Paleozoic Brasiliano Orogenic event in South America. Its evolution is …

Rodinia was initially defined as a long‐lived supercontinent that assembled all the
continental fragments around Laurentia and remained stable from 1000 up to 750 Ma …

At least two supercontinents–Rodinia and Gondwana–have been proposed for the 1200–
500Ma time interval on the basis of stratigraphic, geochronological and paleomagnetic …

The name Ribeira Belt was originally used in a reference to a broad belt of deformed crust,
which strikes subparallel to the southeastern Brazilian coastline. It was originally believed to …