Abstract The Himalayan Orogen consists of two rock packages that parallel the topographic
trend of the mountain belt between the eastern and western syntaxes. To avoid confusion …

Eocene–Oligocene foreland basin was formed in response to the India–Asia collision and
ensuing Himalayan orogenesis. The initial collision during late Paleocene to early Eocene …

GPS data reveal that the Brahmaputra Valley has broken from the Indian Plate and rotates
clockwise relative to India about a point a few hundred kilometers west of the Shillong …

Abstract Iron (Fe) and manganese (Mn) are harmful for human health, if present in a higher
concentration, particularly in groundwater. The results of the study revealed that the …

Earthquake disasters occur mainly due to the collapse of buildings and structures triggered
by ground motions. It is, therefore, important to predict ground-shaking levels in order to …

The ESE-WNW trending Central Indian Tectonic Zone (CITZ) divides the Indian subcontinent
into southern and northern crustal provinces. Its narrow northern belt consists of closed early …

This paper analyses the spatio-temporal trends and variability in annual, seasonal, and
monthly rainfall with corresponding rainy days in Bhilangana river basin, Uttarakhand …

Discontinuity-bounded late Quaternary sequences in the southern Gangetic Plains
(Himalayan Foreland Basin) reflect floodplain aggradation and degradation in response to …

We have used Bouguer gravity anomaly and topography data to determine the equivalent
elastic thickness of the lithosphere, Te in the region of the India–Eurasia collisional system …

Earthquakes beneath the Himalayan collision zone occur at depths between near surface
and around 100 km below sea level. After relocating earthquakes with two one‐dimensional …