In this paper we evaluate the morphotectonics of the area around the Subansiri river in north-eastern India. Research focuses on understanding the impacts on areas experiencing active tectonic deformation. It also explains the variety of kinematics observed in the area from the Miocene to the present. The tectonics can explain some structures related to the extensional tectonics predominant in the region and the development of the minor and major morph structures driven by faults with different kinematics. We developed a morphotectonic evolutionary model for the area based on the morphotectonic analysis and geological mapping. Morphotectonic indices used to evaluate the tectonic activeness in this study are Mountain Front sinuosity Ind...
The basement in Upper Assam foreland basin exhibits a typical flexure pattern. An elongated continuo...
In the present study, we have identified the tectonically active zones along the Island Belt Uplift ...
Cratonic areas experience complex process-response changes due to their operative endogenic and exog...
We discuss the tectono-geomorphic evaluation of the Binta basin (Lesser Himalaya, India) through qua...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
© 2015 Taylor & Francis.ABSTRACT: Neotectonic activity in Mahe (Mayyazhi) river basin and its implic...
Morphotectonics interplays between the landscape development and the tectonics. Usually, the develo...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
The Brahmaputra river basin occupies an area of 580,000 km2 lying in Tibet (China), Bhutan, India an...
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...
International audienceThe active growth of a fault-and-thrust belt in frontal zones of Himalaya is a...
© 2017 Informa UK Limited, trading as Taylor & Francis Group. The effects and influence of tecton...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
Tectonic geomorphology can be explained as the study of landforms produced by tectonic processes, or...
The basement in Upper Assam foreland basin exhibits a typical flexure pattern. An elongated continuo...
In the present study, we have identified the tectonically active zones along the Island Belt Uplift ...
Cratonic areas experience complex process-response changes due to their operative endogenic and exog...
We discuss the tectono-geomorphic evaluation of the Binta basin (Lesser Himalaya, India) through qua...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
© 2015 Taylor & Francis.ABSTRACT: Neotectonic activity in Mahe (Mayyazhi) river basin and its implic...
Morphotectonics interplays between the landscape development and the tectonics. Usually, the develo...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
The Brahmaputra river basin occupies an area of 580,000 km2 lying in Tibet (China), Bhutan, India an...
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...
International audienceThe active growth of a fault-and-thrust belt in frontal zones of Himalaya is a...
© 2017 Informa UK Limited, trading as Taylor & Francis Group. The effects and influence of tecton...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
Tectonic geomorphology can be explained as the study of landforms produced by tectonic processes, or...
The basement in Upper Assam foreland basin exhibits a typical flexure pattern. An elongated continuo...
In the present study, we have identified the tectonically active zones along the Island Belt Uplift ...
Cratonic areas experience complex process-response changes due to their operative endogenic and exog...