The Tethyan metallogenic domain (TMD), as one of the three major domains in the world,
extends over 10000 km from east to west, and has developed several world-class …

The offshore Chinese basins are located in the transition zone from the East Asia to the
Western Pacific plate. The Cenozoic evolution of these basins reflects the geodynamic …

Abstract The India-Asia collision is an outstanding smoking gun in the study of continental
collision dynamics. How and when the continental collision occurred remains a long …

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 origin and drift history of the South Qiangtang block (SQB) is critical to understanding
the internal dimensions and kinematics of the late Paleozoic to early Mesozoic Tethyan …

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 …

Knowing the original size of Greater India is a fundamental parameter to quantify the amount
of continental lithosphere that was subducted to help form the Tibetan Plateau and to …

The long-duration, fast convergence, and imbalance of crustal mass in the India-Asia
collisional system challenge the classical rules of continental dynamics. Here, we calculate …

Defining the original size of Greater India is a critical parameter for reconstructing the
kinematics and timing of the India–Asia collision. Early Cretaceous paleontology-based …

The Sangdanlin section in southern Tibet represents a geologic Rosetta stone to constrain
the initiation of the India–Asia collision from its sedimentary and paleomagnetic records …