The tectonic evolution of the Himalayan collision belt has the following characteristics with the continental crustal accretion, thickening and partial melting at the front of the collision belt and upward curving of deep-level structural boundaries cause
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崔军文.1997.喜马拉雅碰撞带的构造演化[J].地质学报,71(2). Cui Junwen.1997. TECTONIC EVOLUTION OF THE HIMALAYAN COLLISION BELT[J]. Acta Geologica Sinica,71(2).
