Himalaya, confined between Indus and Brahmaputra rivers and little beyond, is a large geodynamic laboratory of nature where orogen is still in youth to early mature phases of evolution. This mountain of geological late continent-continent collision origin has very ancient history perhaps touching the Archean. Giant scale endogenous turmoil thoroughly overhauled terrain mostly within the confines of distinct belts or divisions and spectacularly uplifted the ...
