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 …

Zircon U–Pb geochronology and Hf–O isotope geochemistry of metasedimentary rocks,
orthogneisses, and leucogranites in Garhwal, NW India, provide new insights into the …

Greater India comprises a part of the Indian plate that subducted under Asia to help form the
Tibetan Plateau. Defining the size of the Greater India is thus a key constraint to model the …

The **ukang Mélange of the Yarlung-Zangbo suture zone in south Tibet documents low
efficiency of accretion along the southern active margin of Asia during Cretaceous …

Abstract We carried U‐Pb‐Hf geochronology of the clastic sequence covering upper
Mesozoic‐Cenozoic period. The upper Mesozoic sequence is overlain unconformably by …

The evolution of the Neo-Tethys Ocean had a profound effect on global climate change and
the evolution of life. To better constrain the Cretaceous paleogeographic position of the …

Abstract The Tibetan Himalaya represents the northernmost continental unit of the Indian
plate that collided with Asia in the Cenozoic. Paleomagnetic studies on the Tibetan …

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 latitudinal motion of the Tibetan Himalaya—the northernmost continental unit of the
Indian plate—is a key component in testing paleogeographic reconstructions of the Indian …

The age range of the major intra-plate volcanic event that affected the northern Indian
margin in the Early Cretaceous is here defined precisely by detrital zircon geochronology. U …