碰撞造山带 meaning in Chinese

collision orogens

Evolution of cenozoic collision orogen of north kalimantan and its metallogenesis
东南亚北加里曼丹新生代碰撞造山带演化与成矿
Tectonic evolution of the western segment of the altyn tagh collisional orogen , northwest china
阿尔金碰撞造山带西段的构造特征
Himalayan orogen is by far the youngest and largest active continent - continent collision belt in the world and is the ideal place for studying the plate dynamics of intracontinental convergence and investigating the mechanism responsible for uplift of the plateau
喜马拉雅造山带是世界上目前仍在进行的、最年轻的、规模最大的陆-陆碰撞造山带，是研究陆内汇集过程板块动力学以及探讨高原隆升机制的理想场所。
Through studying about tectonic units established , old plates rebuilded , original basins restored , texture and structure of orogenic belt , mechanism and model of orogeny , it is definded that the type of beishan orogenic belt is continent - accretion arc collosion orogenic belt
通过对造山带构造单元的建立、古板块重建、原型盆地恢复、造山带结构、构造特徵及造山机制和模式的研究，确定北山造山带类型为陆增生弧碰撞造山带。