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 …

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 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 …

Abstract The Paraná Basin represents an important sedimentation episode that occurred in
the south margin of Gondwana during the Paleozoic and Mesozoic. The evolution of the …

Some recent models challenge the position and extension of the assumed oceanic basins
formed through the break-up of Rodinia, and the tectonic processes involved in the …

Stratigraphic, isotopic, and geochronological data from two late Neoproterozoic-aged
conglomerate wedges in the southwest São Francisco craton support the interpretation that …

Abstract The Lower Cretaceous Botucatu Formation records the development of widespread
dry–aeolian desert sedimentation throughout the Paraná Basin in south‐west Gondwana …

Este capítulo faz uma revisão de conceitos e hipóteses apresentados anteriormente acerca
da Bacia do Camaquã (região central do Rio Grande do Sul) à luz de uma série de …

Abstract The Porongos Group is the major component of a fold and thrust belt located in the
central portion of the Dom Feliciano Belt in the Sul-Riograndense Shield, Brazil. In this …