Abstract The Kashmir Basin is filled with Pliocene-Pleistocene fluvio-lacustrine sediments.
On the flank of the Pir Panjal these sediments, called “Lower Karewas”, are covered with …

The Kashmir valley, located in the northwestern Himalayas, provides an intermontane valley
fill comprising unconsolidated fluvio-lacustrine sediments of more than a km thickness …

A sediment core from Pariyaj Lake, from the Vatrak River basin, located at the desert margin
in the Gujarat Alluvial Plains of western India, was investigated in a multidisciplinary aspect …

Events of neotectonic activity during the Late Quaternary in the Kumaun Himalaya have
been responsible for reactivation of faults/thrusts and blockade of ancient drainage resulting …

The Pleistocene represents the youngest period of repeated widespread glaciation and
interglacial intervals of both hemispheres. The Pleistocene–Holocene siliciclastics of the …

ABSTRACT The sediments of Karewa Group (Late Neogene to Quaternary in age) represent
a more than 1300 m thick succession of sand, mud and gravels, extending throughout the …

The stratigraphic record of alternating loess deposits and interbedded paleosol profiles is
interpreted to represent glacial-interglacial cycles in response to orbital forces during …

The loess–paleosol sequences of the Karewa Group preserve a valuable repository of the
Late Quaternary climatic changes and the landscape evolution history of the Karewa Basin …

Twelve samples extracted from silt-rich sediments in intramontane basins (“duns”) in the
Siwalik system in SW Nepal were dated by thermoluminescence. The samples from the …

The late Quaternary loess and loess-like deposits in Kashmir Valley are natural archives that
have preserved paleoclimate and paleoenvironmental records of the region. We present a …