The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …

Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen
include where the India–Asia convergence was accommodated and how the plateau grew …

Reconstructions of the relative positions of the India and Eurasia plates, using recently
revised histories of movement between India and Somalia and between North America and …

The sediment archive, of material eroded from an active tectonic region and stored in
adjacent basins, can provide a valuable record of hinterland tectonism especially when …

We report the first geochemical traverse to integrate U–Pb ages and Hf data on single
detrital zircons with bulk-rock Sm–Nd–Rb–Sr isotopic measurements across the breadth of …

Two end‐member kinematic models of crustal shortening across the Himalaya are currently
debated: one assumes localized thrusting along a single major thrust fault, the Main …

How well do deep-sea sedimentary archives track erosion in upland sources, driven by
climatic change or tectonic forcing? Located on the western edge of South Asian monsoon …

Out-of-sequence deformation in the Himalaya has been caused mainly by thrusting. Out-of-
sequence thrusts, usually north-to NE-dip** foreshear planes, occur inside the Sub …

The Himalayan Metamorphic Front consists of two basinal sequences deposited on the
Indian passive margin, the Mesoproterozoic Lesser Himalayan Sequence and the …