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.
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Jain, A. K., & Bhowmik, S. K. (2016). Tectonics and evolution of the Trans-Himalayan Mountains and Nagaland Ophiolite Belt. In Proceedings of the Indian National Science Academy (Vol. 82, pp. 617–624). Indian National Science Academy. https://doi.org/10.16943/ptinsa/2016/48471
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