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 …

Establishing how tectonic plates have moved since deep time is essential for understanding
how Earth's geodynamic system has evolved and operates, thus answering longstanding …

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 …

This paper presents a brief synthesis of the current state of knowledge on the formation and
break-up of the early-Neoproterozoic supercontinent Rodinia, and the subsequent assembly …

During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS)
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …

The origin of the Antarctic continent can be traced to a relatively small late Archaean cratonic
nucleus centred on the Terre Adélie regions of East Antarctica and the Gawler Craton region …

The assembly of the Gondwana supercontinent during the waning stages of the Proterozoic
provides a tectonic backdrop for the myriad biological, climatological, tectonic and …

Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy
orogens with Ediacaran–Cambrian orogenic belts in Sri Lanka and the Lützow Holm Bay …

The Lhasa terrane in southern Tibet is composed of Precambrian crystalline basement,
Paleozoic to Mesozoic sedimentary strata and Paleozoic to Cenozoic magmatic rocks. This …