This article reconstructs the evolution of the passive northern margin of peninsular India
facing the Neotethys, from the earliest rifting stages in the Carboniferous to final collision …

This review paper deals with the geology of the NW Indian Himalaya situated in the states of
Jammu and Kashmir, Himachal Pradesh and Garhwal. The models and mechanisms …

Rifting processes, leading to sea-floor spreading, are characterized by a sequence of
events: transtensive phase of extension with syn-rift volcanism; simple shear extension …

The geologic evolution of northern India is best recorded in the stratigraphic succession of
the Zanskar Range (northwestern Himalaya), which represents the most complete transect …

The Neo-Tethys Ocean began to form at Early Permian times, when continental flood basalts
were emplaced in various areas of the newly-formed Indian passive margin, exposed today …

Although expanded ocean anoxia has long been believed to be a direct killing mechanism
causing mortality of organisms during the Permian-Triassic mass extinction, little has been …

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 …

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 …

Abstract The Northern part of Great-India underwent an early rifting phase in the late
Paleozoic, just at the end of the large scale Gondwanian glaciation. The beginning of the …

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