The Himalayan orogeny has shaped the sedimentary basins of the region, where
continuous deformation formed both 'conventional'and 'unconventional'petroleum systems at …

This paper presents a review of Late Quaternary climatic changes and glacier variability in
the Himalaya and East Africa, focusing on the role of Indian Summer Monsoon (ISM), East …

Palynological investigation of a 410 cm long core section from Tso Kar (33° 10′ N, 78°
00′ E, 4527 m asl), an alpine lake situated in the arid Ladakh area of NW India at the limit …

Middle to Late Pleistocene loess-paleosol sediments of Kashmir Valley, India, were
analyzed for major, trace and REE elements in order to determine their chemical …

The somewhat abrupt commencement of loess deposition on a large scale in north-central
China is palaeomagnetically measured at about 2.5 Ma. The formation of the dynamical …

The regional climate of the Himalayas is predominated by the southwest monsoons and the
western disturbances. The uplift of the Pir Panjal to its present height is believed to restrict …

This paper focuses on the analysis of geomorphic landform development, particularly
between the Trans Himadri Fault and the Main Central Thrust including Berinag Thrust and …

In the present study, the retreat of Kolahoi glacier was mapped from the satellite
observations and historical maps supplemented by the extensive field observations to …

India collided with mainland Asia at 65 Ma. The pressure rose to 9-11 kbar in the collision
zone. As the Indian lithosphere bent down and its upper crust buckled up as an upwarp in …

Integrating multiproxy results (geochemistry, mineral magnetism, grain size, and C/N ratio
variability supported by 14C AMS dating), obtained from a 1.4-m sediment core retrieved …