Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …

Longitudinal profiles along sixteen major transverse Himalayan rivers add important
constraints to models of active continental subduction and its evolution. These profiles are …

Since the opening of Nepal in 1950, a wealth of new information on the geology of the
Himalaya has emanated from this country. The sedimentary history of the Range is most …

A large number of fractures, faults and folds trending normal and oblique to the Himalayan
tectonic trend have been recognized in recent years. The tear faults of Kumaun and Nepal …

The Himalaya passive margin should be separated into the Indian Himalaya and the
Pakistan Himalaya, divided by the Nanga Parbat-Haramosh basement uplift in the …

The series of four different, steeply inclined thrusts which sharply sever the youthful
autochthonous Cenozoic sedimentary zone, including the Siwalik, from the mature old …

Despite being the largest active collisional orogen on Earth, the growth mechanism of the
Himalaya remains uncertain. Current debate has focused on the role of dynamic interaction …

Bank sediments and suspended loads of the Brahmaputra River and its important tributaries
were collected from the Himalayan front to Bangladesh along with most of the important …

This Monograph Aims To Apprise Readers Of The Natural Events That Occurred And The
Processes That Were In Operation Before The Emergence Of The Giant Edifice Of The …

How plate-boundary processes control intra-continental deformation is a fundamental
question in Earth sciences. Although it is long known that the active India–Asia convergence …