The timing, kinematics, and geodynamic evolution of the India-Asia continental collision are
crucial to understanding the geological and geomorphological evolution of the Himalayan …

The timing and magnitude of the early Cenozoic surface uplift of the Tibetan Plateau is
controversial due to a scarcity of unaltered terrestrial sediments required for palaeoaltimetry …

The forms of the margins of the Lhasa terrane and the Tethyan Himalaya prior to the
collision of India and Eurasia as constrained by paleomagnetism are ambiguous due to the …

The precollisional location and shape of the Lhasa terrane are crucial for constraining the
closure of the Neo-Tethys Ocean and the ensuing India-Asia collision; however, estimation …

Abstract The India‐Eurasia collision is a key case study for understanding the influence of
plate tectonic processes on Earth's crust, atmosphere, hydrosphere, and biosphere …

Abstract The Paleocene lavas from Dianzhong Formation (E1d) in Linzhou basin of southern
Lhasa terrane are a key target for paleomagnetic investigations into the timing and …

The drift history of the Lhasa terrane from Gondwana to Asia plays a crucial role in
understanding the Tethys evolution and true polar wander (TPW). However, few reliable …

Abstract The Late Cretaceous and Paleogene sediments from the Tethyan Himalaya can
provide paleomagnetic constraints on the pre-collision size of Greater India. However …

Abstract Interpretations of pre-collisional configurations of Greater India are highly
controversial and predict distinct processes during the India-Asia collision. To better …

Abstract The India-Asia collision processes are under current debate, mainly due to the
large variations of the pre-collision position of the southern margin of Asia, in the range of 10 …