Pangea is the youngest supercontinent in Earth's history and its main body formed by
assembly of Gondwana and Laurasia about 300–250 Ma ago. As supported by voluminous …

Neoproterozoic tectonic geography was dominated by the formation of the supercontinent
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …

The making of Pangea is the result of large-scale amalgamation of continents and micro-
continents, which started at the end of the Neoproterozoic with the formation of Gondwana …

Just over 15 years ago, a proposal forwarded by Rogers and Santosh (2002) posited the
existence of a pre-Rodinia supercontinent which they called Columbia. The conjecture …

Abstract The Wilson Cycle theory that oceans close and reopen along the former suture is a
fundamental concept in plate tectonics. It was named after J. Tuzo Wilson who recognised …

The Precambrian geologic history of Peninsular India covers nearly 3.0 billion years of time.
India is presently attached to the Eurasian continent although it remains (for now) a separate …

Stratigraphic, geochronologic, and geochemical patterns of Neoproterozoic to Cambrian
sedimentary and volcanic rocks in Utah, Nevada, and SE Idaho record a dynamically …

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

Geological, geochronological and isotopic data are integrated in order to present a revised
model for the Neoproterozoic evolution of Western Gondwana. Although the classical …

The Neoproterozoic to Early Cambrian amalgamation of SW Gondwana through the
Brasiliano/Pan-African orogeny is reviewed with emphasis on the role of the Río de la Plata …