Southward orogenic growth of the Himalaya, since the Eocene led to variable crustal
loading, flexural subsidence and foreland basin sedimentation. Structural adjustments …

An understanding about lithology, tectonics and unroofing history of provenance is mostly
drawn from the compositional and textural parameters of the detrital fragments. We here use …

The geochemical and petrological studies were carried out to deduce the chemical
composition, provenance, and intensity of chemical weathering of the source rocks in the …

Two main geodynamic processes have controlled evolution of the Himalaya, Trans-
Himalayan and Karakoram terrains due to underthrusting of the Indian Plate beneath the …

The fluviatile succession of Siwalik Group of the Himalayan Foreland Basin (Siwalik Group)
represents one of the largest and active basins that have recorded the various manifestation …

Various lithofacies from Boulder Conglomerate Formation of the Upper Siwalik Subgroup
exposed around village Kangar in Jammu District are described to understand the …

Late Quaternary fluvial deposits along the Janauri (JA; comprises Siwalik rocks) and Bhaddi
(BA; dominantly of Quaternary deposits) anticlines over independent fault segments of the …

Following crustal thickening in the Lesser Himalaya subprovince, particularly along its
southern margin due to bending down of the crust, a flexural depression developed …

Himalayan orogen is the result of collision and ongoing convergence of India and Eurasia
since~ 55 Ma. The Siwalik Group, at the foot of the Himalaya formed during the Miocene as …

The foreland basin is the southernmost part of the Himalaya. It is separated from the Indo-
Gangetic Alluvial Plain by the Himalayan Frontal Thrust (HFT). The HFT is an active thrust …