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Metamorphic core complexes: Windows into the mechanics and rheology of the crust
Metamorphic core complexes are products of normal-fault displacements sufficient to
exhume rocks from below the brittle–ductile transition. These faults (detachments) may …
exhume rocks from below the brittle–ductile transition. These faults (detachments) may …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
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 …
geological framework and initial growth were fundamentally the result of multiple, previous …
Cenozoic tectonic evolution of Asia: A preliminary synthesis
Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
Active tectonics of Himalayan frontal fault system
Abstract In the Sub-Himalayan zone, the frontal Siwalik range abuts against the alluvial plain
with an abrupt physiographic break along the Himalayan Frontal Thrust (HFT), defining the …
with an abrupt physiographic break along the Himalayan Frontal Thrust (HFT), defining the …
Active structures of the Himalayan-Tibetan orogen and their relationships to earthquake distribution, contemporary strain field, and Cenozoic volcanism
We have compiled the distribution of active faults and folds in the Himalayan-Tibetan orogen
and its immediate surrounding regions into a web-based digital map. The main product of …
and its immediate surrounding regions into a web-based digital map. The main product of …
Restoration of Cenozoic deformation in Asia and the size of Greater India
A long‐standing problem in the geological evolution of the India‐Asia collision zone is how
and where convergence between India and Asia was accommodated since collision …
and where convergence between India and Asia was accommodated since collision …
Cenozoic tectonic history of the Himachal Himalaya (northwestern India) and its constraints on the formation mechanism of the Himalayan orogen
A central debate for the evolution of the Himalayan orogen is how the Greater Himalayan
Crystalline complex in its core was emplaced during the Cenozoic Indo-Asian collision …
Crystalline complex in its core was emplaced during the Cenozoic Indo-Asian collision …
Lateral constrictional flow of hot orogenic crust: Insights from the Neoarchean of south India, geological and geophysical implications for orogenic plateaux
This study provides an in situ geological perspective on fabrics produced by
synconvergence lateral crustal flow of hot orogens. It is based on the example of the …
synconvergence lateral crustal flow of hot orogens. It is based on the example of the …
Tectonic evolution of the Himalayan thrust belt in western Nepal: Implications for channel flow models
We present a new geologic map of western Nepal and three balanced regional cross
sections in the Himalayan thrust belt. The minimum shortening between the South Tibetan …
sections in the Himalayan thrust belt. The minimum shortening between the South Tibetan …
Late Pliocene onset of the Cona rift, eastern Himalaya, confirms eastward propagation of extension in Himalayan-Tibetan orogen
Several competing hypotheses have been proposed to explain east-west extension
observed across the Himalayan orogen, based primarily on observations from the western …
observed across the Himalayan orogen, based primarily on observations from the western …