Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

This study seeks to determine the ultimate origin of aeolian sand in Arabian deserts by high-
resolution petrographic and heavy-mineral techniques combined with zircon U–Pb …

As the chronicle of plate motions through time, paleogeography is fundamental to our
understanding of plate tectonics and its role in sha** the geology of the present-day. To …

We studied the stratigraphy, composition, and paleomagnetic properties of lateritic
weathering profiles of Permian age from northern Iran and western Karakoram, Pakistan. A …

A well-justified stratigraphical correlation of continental successions and new
palaeogeographic reconstruction of Pangaea reveal new insights into the northern …

The Turkish part of the Tethyan realm is represented by a series of terranes juxtaposed
through Alpine convergent movements and separated by complex suture zones. Different …

The geographical location of the Lhasa terrane in the Permian remains a subject of debate.
The recognition of the Permian basalts in the Tethyan Himalaya and the Permian volcanic …

The pre-drift Wegenerian model of Pangea is almost universally accepted, but debate exists
on its pre-Jurassic configuration since Ted Irving introduced Pangea 'B'by placing …

Atmospheric CO2 is thought to play a fundamental role in Earth's climate regulation. Yet, for
much of Earth's geological past, atmospheric CO2 has been poorly constrained, hindering …

The evolution of the Neo-Tethys realm had a significant impact on the Phanerozoic
paleogeography of the Iran Plateau. However, there remains significant debate regarding …