The Himalaya–Karakoram–Tibet mountain belt resulted from Cenozoic collision of India and Asia and is frequently used as the type example of a continental co
Papers from a symposium held in San Antonio, Texas, 1986. Contributors consider problems of crustal and lithospheric scales in this area. Contains a folded map
The Himalayan mountain belt, which developed during the India–Asia collision starting about 55 Ma ago, is a dramatically active orogen and it is regarded as t