Abstract The Dom Feliciano Belt evolution is reviewed based on cross-sections, space–time
diagrams, PT paths, and Sr–Nd isotopic data of pre-collisional metaigneous rocks. The belt …

The amalgamation of southwestern Gondwana during the late Neoproterozoic
Brasiliano/Pan-African orogenic cycle involved the tectonic interaction of the Congo …

In considering the geology of Western Gondwana, this text covers: the Pan-African-
Brasiliano cratons; the Pan-African-Brasiliano fold belts; and amosaic of Pan-African …

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 …

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 …

Gondwana resulted from accretion of fragments of the Rodinia supercontinent. However,
precise times and circumstances of individual accretions are still disputed. Aggregation of …

Abstract The Dom Feliciano Belt is an orogenic association that extends from southern Brazil
to Uruguay parallel to the Atlantic coastline for over 1100 km. It was assembled in the …

Juvenile, mantle-derived complexes are relatively rare in the late Neoproterozoic Brasiliano
orogenic belts of western Gondwana, which consist primarily of reworked older crust. The …

The new Geodynamic Map of Gondwana Supercontinent Assembly provides insight onto the
Neoproterozoic breakup of the Rodinia supercontinent that existed from 1000 to 725 Ma …

The Brasiliano Cycle in southern Brazil and Uruguay is represented by three major NE-SW
trending geotectonic units: the Vila Nova belt, Tijucas belt and Dom Feliciano belt. The Vila …