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 …

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

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Tectonic models for the Oligocene–Miocene development of the Himalaya mountain range
are largely focused on crustal-scale processes, and developed along orogen-perpendicular …

Abstract The Himalayan Orogen consists of two rock packages that parallel the topographic
trend of the mountain belt between the eastern and western syntaxes. To avoid confusion …

Both climatic and tectonic processes affect bedrock erosion and exhumation in convergent
orogens, but determining their respective influence is difficult. A requisite first step is to …

A line-length balanced palinspastic reconstruction across the Himachal Himalaya is
presented, highlighting different phases of Himalayan tectonic development: Eocene …

The Himalaya consists of thrust sheets tectonically shingled together since~ 58 Ma as India
collided with and slid beneath Asia. Major Himalayan structures, including the South Tibetan …

Advancements in thermochronology and numerical modeling offer the potential to associate
the age of thermochronometric samples to both exhumational and deformational processes …

Abstract The Higher Himalayan Crystalline (HHC) in the Bhagirathi river section (India) on
fieldwork reveals two extensional ductile top-to-N/NE shear sub-zones—the 'South Tibetan …