Tectonics and Evolution of the Trans-Himalayan Mountains and Nagaland Ophiolite Belt

  • A K JAIN CSIR-Central Building Research Institute, Roorkee

Abstract

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.

Published
2017-02-09