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 …

The morphotectonic study was carried out in the Nahan salient, located between the well
known Kangra and Dehradun recesses in western Himalaya, India. We used various …

In this paper, we report geomorphic signatures of neotectonic activity identified from the area
around Nahan Salient along Himalayan Frontal Thrust (HFT), using remote sensing and …

The Himalayan front exhibits varying convergence rates along its length. This study
examines the morphotectonic evolution of the landforms in an intermontane valley (viz …

Previous studies have identified a seismic gap that has not witnessed any surface rupture
earthquakes in the last 200–500 years located in the central sub-Himalaya (ie, area around …

Thrusting supports the development of diverse landforms and deformational structures in the
Himalayan Frontal Thrust (HFT) region between Kathgodam and the Chorgallia sector …

This overview provides a review of the development of luminescence dating in India,
recounts important contributions and their import on the chronology of the Indian Quaternary …

Channel width is an important parameter of the hydraulic geometry of a river and can be
linked to the tectonic, topographic, lithologic, and climatic controls in a particular reach. As …

Depositional river terraces in tectonically active regions are used to determine the relative
roles of tectonic and climatic changes in the landscape evolution of an area. Apart from …

Geomorphic features can be used to retrieve and evaluate active tectonic features in tectonic
orogens and data can be easily generated from coarse resolution DEMs (SRTM, ASTER) …