The extent and nature of the Archaean–Palaeoproterozoic craton of Río de la Plata of
southern South America, a major but poorly understood crustal component in …

The southernmost outcrops of the Río de la Plata cratonic region are exposed in the Tandilia
System in eastern Argentina. The geological evolution comprises mainly an igneous …

Four main classes of tectonic entities may be considered for the Ribeira Belt and southwest
African counterparts:(1) cratonic fragments older than 1.8 Ga and their passive margin …

Abstract Neoproterozoic–Cambrian amalgamation of West Gondwana involved the collision
of several terranes of older crust that are now in eastern South America and western Africa …

Our current understanding of the tectonic history of the principal Pan-African orogenic belts
in southwestern Africa, reaching from the West Congo Belt in the north to the …

Gondwana was consolidated in the late Cambrian after 180 myr of tectonic convergence
among Neoproterozoic paleocontinents and smaller fragments. We present a compilation of …

Abstract The Neoproterozoic-Eoplalaeozoic Brasiliano orogeny at the eastern margin of the
Rio de la Plata craton in southernmost Brazil and Uruguay comprises a complex tectonic …

Strontium and carbon isotopes of marine carbonates are routinely applied for
chemostratigraphic cross correlations of time-equivalent sedimentary sequences and for …

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

Although the Río de la Plata craton is exposed over a relatively large area in Uruguay,
eastern Argentina, and southernmost Brazil, its geological evolution is poorly known …