A review on out-of-sequence deformation in the Himalaya
S Mukherjee - Special Publications, 2015 - lyellcollection.org
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 …
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
Kinematic evolution of a continental collision: Constraining the Himalayan-Tibetan orogen via bulk strain rates
We investigated temporal variations of the bulk strain rate across the Himalayan-Tibetan
orogen, which impact the magnitudes, rates, and distribution of deformation across the …
orogen, which impact the magnitudes, rates, and distribution of deformation across the …
[PDF][PDF] Non-emergent thrust front along the northwest Jammu Sub-Himalaya: evidence from channel profile analysis across the Surin Mastgarh Anticline
A Aravind, R Devrani, R Jayangondaperumal… - Himal. Geol …, 2022 - researchgate.net
The Himalayan Frontal Thrust (HFT) is emergent throughout the central and NE Himalayas.
The emergent thrust creates an anticline structure in its hanging wall, and they are either …
The emergent thrust creates an anticline structure in its hanging wall, and they are either …
Evaluation of seismically induced Soft Sediment deformation structures vis-a-vis their probable earthquake sources in Kashmir basin, NW Himalaya
This study discusses the composition and distribution of paleo-liquefaction structures, their
triggering mechanisms, probable source and the dynamics of source faults expressed in the …
triggering mechanisms, probable source and the dynamics of source faults expressed in the …
Comment on:“Earthquake geology of Kashmir Basin and its implications for future large earthquakes” by Shah (2013);“Kashmir Basin Fault and its tectonic …
S Ahmad, A Alam, B Ahmad - International Journal of Earth Sciences, 2016 - Springer
Accepted: 7 August 2015/Published online: 5 September 2015© Springer-Verlag Berlin
Heidelberg 2015 (KBF) without any additional structural, kinematic, geologic or geomorphic …
Heidelberg 2015 (KBF) without any additional structural, kinematic, geologic or geomorphic …
Segmentation of main boundary thrust and main central thrust in western Himalaya for assessment of seismic hazard by Mridula et al., Nat Hazards (2016) 84: 383 …
AA Shah, SM Talha Qadri - Natural Hazards, 2017 - Springer
Abstract Mridula et al.(Nat Hazards 84: 383–403,(2016) have tried to identify segments of
two major thrust faults, the Main Boundary Thrust and Main Central Thrust, in Western …
two major thrust faults, the Main Boundary Thrust and Main Central Thrust, in Western …
Structural variations in basal decollement and internal deformation of the Lesser Himalayan duplex trigger landscape morphology in NW Himalayan interiors
S Dey, R Thiede, A Biswas… - Earth Surface …, 2020 - esurf.copernicus.org
The Kishtwar Window (KW) of the NW Himalaya exposes the northwestern termination of the
orogen-parallel anticlinal stack of thrust nappes, termed as the Lesser Himalayan Duplex …
orogen-parallel anticlinal stack of thrust nappes, termed as the Lesser Himalayan Duplex …
[PDF][PDF] Growth of the Lesser Himalayan Duplex and rapid fluvial incision modulate landscape morphology in tectonically-active Kishtwar Window in NW Himalayan …
Abstract The Kishtwar Window (KW) of the NW Himalaya exposes the north-western
termination of the orogen-parallel anticlinal stack of thrust nappes, known as the Lesser …
termination of the orogen-parallel anticlinal stack of thrust nappes, known as the Lesser …