International audienceThe active growth of a fault-and-thrust belt in frontal zones of Himalaya is a prominent topographical feature, extending 2500 km from Assam to Pakistan. In this paper, kinematical analysis of frontal anticlines and spatial mapping of active faults based on geomorphological features such as drainage pattern development, fault scarps and uplifted Quaternary alluvial fans are presented. We analyse the geomorphic and hydrographic expressions of the Chandigarh and the Janauri active anticlines in the NW India Siwaliks. To investigate the morphological scenario during the folding process, we used spatial imagery, geomorphometric parameters extracted from digital elevation models and fieldwork. The approach presented here in...
Landscapes in tectonically active Hindu Kush (NW Pakistan and NE Afghanistan) result from a complex ...
In this paper we evaluate the morphotectonics of the area around the Subansiri river in north-easter...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
International audienceThe active growth of a fault-and-thrust belt in frontal zones of Himalaya is a...
The 100 km long frontal foreland fold-the Janauri anticline in NW Himalayan foothills represents a s...
Fold topography preserves a potentially accessible record of the structure and evolution of an under...
International audienceThe aim of this contribution is to show the styles of growing anticlines and t...
The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evid...
We discuss the tectono-geomorphic evaluation of the Binta basin (Lesser Himalaya, India) through qua...
The morphotectonic study was carried out in the Nahan salient, located between the well known Kangra...
The morphotectonic studies help in deciphering the role of tectonics and neotectonics in morphologic...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
The Kumaun Sub-Himalaya region is one of the most active regions falling into Seismic Zone V along t...
Numerous newly-identified traces of active faults in the Himalayan foothill zone along the HFF aroun...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
Landscapes in tectonically active Hindu Kush (NW Pakistan and NE Afghanistan) result from a complex ...
In this paper we evaluate the morphotectonics of the area around the Subansiri river in north-easter...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
International audienceThe active growth of a fault-and-thrust belt in frontal zones of Himalaya is a...
The 100 km long frontal foreland fold-the Janauri anticline in NW Himalayan foothills represents a s...
Fold topography preserves a potentially accessible record of the structure and evolution of an under...
International audienceThe aim of this contribution is to show the styles of growing anticlines and t...
The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evid...
We discuss the tectono-geomorphic evaluation of the Binta basin (Lesser Himalaya, India) through qua...
The morphotectonic study was carried out in the Nahan salient, located between the well known Kangra...
The morphotectonic studies help in deciphering the role of tectonics and neotectonics in morphologic...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
The Kumaun Sub-Himalaya region is one of the most active regions falling into Seismic Zone V along t...
Numerous newly-identified traces of active faults in the Himalayan foothill zone along the HFF aroun...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
Landscapes in tectonically active Hindu Kush (NW Pakistan and NE Afghanistan) result from a complex ...
In this paper we evaluate the morphotectonics of the area around the Subansiri river in north-easter...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...