Tectono-magmatic evolution of Tethyan oceanic lithosphere in supra subduction zone fore arc regime:G

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The Naga Hills Ophiolite(NHO)belt in the Indo-Myanmar range(IMR)represents a segment of Tethyan oceanic crust and upper mantle that was involved in an eastward convergence and collision of the Indian Plate with the Burmese Plate during the Late Cretaceous
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