The Qilian orogenic system in the northern Tibetan Plateau records the complete tectonic
cycle from opening of Proto-Tethys Ocean, initial subduction, to continental subduction and …

The enigmatic geodynamic processes involved in the India-Asia collision shape our
understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes …

The timing of continental collision between India and Asia has been controversial for a long
time because of the difficulty in screening isotopic ages for different types of tectonothermal …

The character of arcs varies over time with significant temporal fluctuations in the quantity
and spatiotemporal patterns of magmatism. However, the driving mechanisms for this …

Southeast Asia is located at the intersection of the Tethys and Pacific domains. The
superimposed effects of the two tectonic domains have resulted in complicated deep …

We integrated our new data with a review of published work on the Indo-Myanmar Orogenic
Belt (IMOB) of the eastern Neotethys in Myanmar, western Yunnan (China) and Naga Hills …

Abstract Knowledge of the size of Greater India is critical to deciphering the geodynamic
processes of the India-Asia collision, as the size of this landmass primarily determines the …

Tethys tectonic system has experienced a long-term evolution history, including multiple
Wilson cycles; thus, it is an ideal target for analyzing plate tectonics and geodynamics …