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型花岗岩的发育是造山运动结束的标志。A type granitoids are the indicator of the end of orogenesis.

产生于板块碰撞后隆起到造山晚期的构造背景。They occurred under the tectonic setting ranging from post collision uplift to late orogenesis.

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板块构造活动，特别是陆内造山作用是热液金成矿作用的原动力。Original dynamical power was resulted from plate tectonic activities, especially from intracontinental orogenesis.

根据金矿脉与后期岩脉伴生的特征，矿化可能发生在中生代燕山期。All these events occurred in Yanshanian period, which has been considered as the post-orogenic period of the Indosinian Orogenesis.

岩浆的侵入对造山变形有重要影响，同时也是导致区域非线性变形的重要地质过程和因素。The intrusion of magma affected the orogenesis and deformation and it is an important geological process and factor leading nonlinear deformation.

该区的碰撞造山作用主要发生在石炭纪和二叠纪，并经历了先挤压后伸展的演化过程。The collisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension.

阿尔泰造山带主要形成于晚泥盆世至早二叠世的主造山期，为一冲断-推覆-滑脱的造山作用。The Altay orogenic belt, in Xinjiang, China was formed mainly during late Devonian to early Permian and was mainly a thrust-nappe-detachment orogenesis.

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巴罗型中压变质带与巴肯型低压高温变质带的成因与大陆板块边缘的碰撞造山及陆内造山作用之间有着紧密的联系。The origins of barrovian type and buchan type of metamorphism are commonly associated with orogenesis at continental collisional margins or within plates.

长江流域的地质-生态环境与自然灾害受到中新生代以来地壳运动和秦岭-大别等造山作用的严格制约与影响。Natural disasters and eco-environment in the Yangtze Valley have been restricted and impressed by crustal movement and Qinling-Dabie orogenesis since the Mesozoic and Cenozoic.

新疆北部浅成低温热液型金矿主要产在碰撞造山带拉张环境浅海相、海陆交互相地层内，是长期多次热液活动的结果。The epithermal gold deposits in the northern Xinjiang are hosted in marine and marine continental strata which were deposited under extensional environment of collision orogenesis.

评述了板块构造“登陆”以来的多岛洋构造、板内造山多岛海模式以及多岛弧盆系构造在造山带研究中的重要性。The paper presents a review of the value of archipelagic ocean model, archipelago model of intraplate orogenesis and composite arc-basin system tectonics since plate tectonic landing.

基于分析陆内俯冲过程物质的活化迁移规律建立了碰撞造山成岩成矿模式，认为仰冲板片上依次出现热液矿床带、花岗岩基带和斑岩带。Based on analysis of activation and outward movement of materials of the intracontinental subducting slab, the petrogenic and metallogenic model was established for collision orogenesis.