This paper reviews the spatial-temporal distribution, geological and geochemical features,
and geophysical context of diverse types of Cenozoic ore deposits formed during India …

In this study, we integrate bedrock datasets, observations of subducted slabs in the mantle,
and plate kinematic constraints to constrain models for the India-Asia collision and the …

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 …

The formation of the Himalaya was associated with the exhumation of high-grade
metamorphosed rocks of the Higher Himalayan sequence (HHS) complex, which underwent …

The zirconium-in-rutile thermometer enjoys widespread use, but confidence in its accuracy
is limited because experiments were conducted at higher temperatures than many rutile …

Despite several decades of investigations, the nature and timing of the India–Asia collision
remain debated. In the western Himalaya, the leading edge of the Indian continent was …

Widespread anatexis was a regional response to the evolution of the Himalayan‐Tibetan
Orogen that occurred some 30 Ma after collision between Asia and India. This paper reviews …

The largest crystalline unit representing the mid-crust in the Himalayan belt is the Greater
Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …

Partial melting is thought to profoundly impact the rheology and deformation behavior of the
middle crust. Consequently, investigations of the pressure-temperature conditions of …

The Himalayan orogen is an archetype of collisional orogens built by the continental
collision between India and Asia in the Cenozoic, and it has been a natural laboratory for …