Paleogeography is the study of the changing surface of Earth through time. Driven by plate
tectonics, the configuration of the continents and ocean basins has been in constant flux …

Recent progress in plate tectonic reconstructions has seen models move beyond the
classical idea of continental drift by attempting to reconstruct the full evolving configuration of …

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 …

Abstract The East African Orogen, extending from southern Israel, Sinai and Jordan in the
north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …

Abstract After its Ediacaran-Early Cambrian assembly, Gondwana was flanked by a system
of peripheral orogens, Terra Australis, Avalonian-Cadomian and newly defined North Indo …

Detrital zircon data have recently become available from many different portions of the
Tibetan–Himalayan orogen. This study uses 13,441 new or existing U‐Pb ages of zircon …

Phanerozoic primary tin and tungsten deposits and lithium–cesium–tantalum (LCT) type
pegmatites define discontinuous belts that reach several thousand kilometers length …

The continental crust is unique to the Earth in the solar system, and controversies remain
regarding its origin, accretion and reworking of continents. The plate tectonics theory has …

Abstract Both the Borborema Province of NE Brazil and the geological provinces of NW
Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and …