Scientific investigations in the Trans-Himalayan and Nagaland ophiolite belt during the period 2011-2015 incorporated various geological and geophysical aspects of evolution of these mountains, including large-scale tectonics of the Indian Plate, its sub-surface configuration, structure and metamorphism. Certain remote areas of Karakoram along the upper Shyok valley and Nagaland were covered for their metamorphism and high pressure metamorphism of ophiolite belts, respectively
Sillimanite- and staurolite-grade metamorphic rocks exhumed along the Pangong fault, the NE branch o...
Abstract: The Nubra-Shyok confluence in northern Ladakh is a key area for understanding the tectonic...
The eastern Karakoram terrane, NW India, records crustal evolution in the core of the Himalayan–Tibe...
The Tso Morari nappe is well known for having suffered ultrahigh-pressure metamorphism in the northw...
The closing of the Tethys Ocean and continent-continent collision along the Alpine-Himalayan chain u...
Abstract: Highly disrupted and deformed slices of ophiolitic rocks occurring along a linear belt in ...
The tectonic significance of blueschist-facies rocks associated with the Indo-Myanmar ophiolite belt...
This thesis attempts to construct an integrated model for the tectonothermal evolution of the Suru v...
Eclogite from two locations in a fossil accretionary complex now exposed in Nagaland, NE India, at t...
Following the c. 50 Ma India–Kohistan arc–Asia collision, crustal thickening uplifted the Himalaya (...
The Himalaya originated as a result of subduction of the Tethyan oceanic crust that lay between Indi...
Metamorphic rocks constitute a vast volumetric proportion of the Earth’s continental lithosphere and...
AbstractThe eastern Karakoram terrane, NW India, records crustal evolution in the core of the Himala...
The pre-collisional tectonic evolution of the north Indian continental margin is best recorded in th...
The Himalayan orogen has experienced intense Cenozoic deformation and widespread metamorphism, makin...
Sillimanite- and staurolite-grade metamorphic rocks exhumed along the Pangong fault, the NE branch o...
Abstract: The Nubra-Shyok confluence in northern Ladakh is a key area for understanding the tectonic...
The eastern Karakoram terrane, NW India, records crustal evolution in the core of the Himalayan–Tibe...
The Tso Morari nappe is well known for having suffered ultrahigh-pressure metamorphism in the northw...
The closing of the Tethys Ocean and continent-continent collision along the Alpine-Himalayan chain u...
Abstract: Highly disrupted and deformed slices of ophiolitic rocks occurring along a linear belt in ...
The tectonic significance of blueschist-facies rocks associated with the Indo-Myanmar ophiolite belt...
This thesis attempts to construct an integrated model for the tectonothermal evolution of the Suru v...
Eclogite from two locations in a fossil accretionary complex now exposed in Nagaland, NE India, at t...
Following the c. 50 Ma India–Kohistan arc–Asia collision, crustal thickening uplifted the Himalaya (...
The Himalaya originated as a result of subduction of the Tethyan oceanic crust that lay between Indi...
Metamorphic rocks constitute a vast volumetric proportion of the Earth’s continental lithosphere and...
AbstractThe eastern Karakoram terrane, NW India, records crustal evolution in the core of the Himala...
The pre-collisional tectonic evolution of the north Indian continental margin is best recorded in th...
The Himalayan orogen has experienced intense Cenozoic deformation and widespread metamorphism, makin...
Sillimanite- and staurolite-grade metamorphic rocks exhumed along the Pangong fault, the NE branch o...
Abstract: The Nubra-Shyok confluence in northern Ladakh is a key area for understanding the tectonic...
The eastern Karakoram terrane, NW India, records crustal evolution in the core of the Himalayan–Tibe...