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 …
Application of modern geomorphic concepts for understanding the spatio-temporal complexity of the large Ganga river dispersal system
Significant advances have been made towards understanding the dynamics of geomorphic
systems through the development of new concepts. In the last two decades, these …
systems through the development of new concepts. In the last two decades, these …
Identification of groundwater potential zones using remote sensing and GIS of KJ Watershed, India
BS Chaudhary, S Kumar - Journal of the Geological Society of India, 2018 - Springer
Groundwater potential zone mapping has become easier with the inputs from Remote
Sensing (RS) & Geographical Information System (GIS) techniques. Various thematic maps …
Sensing (RS) & Geographical Information System (GIS) techniques. Various thematic maps …
Longitudinal profiles and geomorphic indices analysis on tectonic evidence of fluvial form, process and landform deformation of Eastern Himalayan Rivers, India
S Ayaz, MK Dhali - Geology, Ecology, and Landscapes, 2020 - Taylor & Francis
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear
indicators of the active orogenic belt of most recent origin formed by the collision of Indian …
indicators of the active orogenic belt of most recent origin formed by the collision of Indian …
Geometry and kinematics of Main Frontal thrust-related fault propagation folding in the Mohand Range, northwest Himalaya
Abstract The Main Frontal thrust (MFT) shapes the∼ 2500 km-long frontal Himalayan arc
between two syntaxes. Surprisingly, the structural geometry and kinematics of the MFT sheet …
between two syntaxes. Surprisingly, the structural geometry and kinematics of the MFT sheet …
[HTML][HTML] Seismic imaging of the Main Frontal Thrust in Nepal reveals a shallow décollement and blind thrusting
Because great earthquakes in the Himalaya have an average recurrence interval exceeding
500 yr, most of what we know about past earthquakes comes from paleoseismology and …
500 yr, most of what we know about past earthquakes comes from paleoseismology and …
Quaternary deformation in the Gorubathan recess: Insights on the structural and landscape evolution in the frontal Darjiling Himalaya
The Gorubathan recess in the Darjiling frontal Himalaya is an unusual and unique region in
the Himalaya as the Ramgarh thrust (RT) rather than the MFT defines the mountain front and …
the Himalaya as the Ramgarh thrust (RT) rather than the MFT defines the mountain front and …
Interplay between faulting and base level in the development of Himalayan frontal fold topography
JB Barnes, AL Densmore, M Mukul… - Journal of …, 2011 - Wiley Online Library
Fold topography preserves a potentially accessible record of the structure and evolution of
an underlying thrust fault system, provided we understand the factors that shape that …
an underlying thrust fault system, provided we understand the factors that shape that …
Morphotectonic analysis of alluvial fan dynamics: comparative study in spatio-temporal scale of Himalayan foothill, India
S Ayaz, M Biswas, MK Dhali - Arabian Journal of Geosciences, 2018 - Springer
Alluvial fan is a depositional fluvial landform that is characterised by sediment flow and
hydrological processes and is also controlled by tectonic activity. These extraordinary …
hydrological processes and is also controlled by tectonic activity. These extraordinary …
Morpho-sedimentary characteristics of the Quaternary Matiali fan and associated river terraces, Jalpaiguri, India: Implications for climatic controls
R Kar, T Chakraborty, C Chakraborty, P Ghosh… - Geomorphology, 2014 - Elsevier
The Matiali fan is a coarse-grained, small alluvial fan in the eastern Himalayan foothills. It co-
exists side by side with the large Tista megafan and other Quaternary fluvial deposits, and …
exists side by side with the large Tista megafan and other Quaternary fluvial deposits, and …