Beishan orogenic belt passed complex geological evolution by multistage plate divergence - subduction - collision - fitting , with the characteristics of ploycycle multiple orogeny 摘要北山造山带经历多期次、多阶段的板块裂解俯冲碰撞拼合的复杂地质演化历程，具多旋回复合造山的特色。
The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny , and the danxian granite were formed at the latest orogenic phase 琼中岩基可能形成于“印支期”碰撞造山运动峰期后的松弛阶段，而儋县岩基则可能形成于造山运动的结束阶段。
The plumbum of ores belongs to the orogenic belt plumbu m , essentially is the mixture plumbum of earth ' s mantle and crust . the pl umbum originates from the orogenic belt and the metallization has relationship with the orogeny 矿石铅既具有地幔铅的特征，又具有上地壳铅的特征，并且具有造山带铅的特点，成矿作用与造山作用关系密切，铅来源于造山带物质，本质上是壳幔混合铅。
And then a new basin system comes into being . the yanshan erogenic belt is a mesozoic intracratonic erogenic belt . there are several basin - mountain transforming processes in the orogeny , and this paper will discuss this process based on basin evolution 燕山造山带是一个中新生代陆内造山带，在其造山过程中存在多次盆地的形成与消失，本文旨在通过对盆地系统演化的研究来探讨造山过程。
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。
Kashan block of iran is the first oversea risk exploration block of chinese petrochemical co . ltd . kashan block is located in the south - west edge of iranian basin . on the structure , it belongs to alpines - himalayan orogeny belt controlled by dynamic system of tethys - indian ocean 伊朗卡山探区是中石化海外的第一块风险勘探区块，位于中伊朗盆地西南边缘，构造上属于特提斯?印度洋动力体系作用控制的喜马拉雅-阿尔卑斯造山带。
Four tectonic evolution phases have been made out in this area . they are original crust formed in the archean - early proterozoic era , continental crust shearing in the middle - new proterozoic era , plate tectonic developed in sinian - triassic period and intracontinental orogeny in the middle cenozoic period 将区内构造演化归纳为太古?早元古代原始地壳形成、中新元古代大陆地壳裂解、震旦?三叠纪板块构造体制、中新生代陆内造山等四个演化阶段。
The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution . the basins located in the southern margin of the yangtze plate , in the basin dynamic computer simulation , is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt 在沉积盆地分析方面，基本查明扬子板块东南边缘早古生代被动大陆边缘沉积特征及沉积构造演化，同时运用反剥法技术对扬子板块东南大陆边缘沉积盆地形成，演化的构造沉降动力学进行探讨，运用计算机模拟方法，定量动力沉积学对扬子东南边缘奥陶纪到志留纪前陆地进行计算机模拟分析，探索并建立这个古老造山带前陆盆定量参数和动态定量模拟。
Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward , which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure 讨论了查干凹陷及邻区中-新生代盆地构造演化及其地球动力学特征，三叠纪(印支期)为陆内造山作用与地壳增厚、隆升剥蚀阶段；侏罗纪(燕山早期)为造山后造山带的局部伸展垮塌阶段；白垩纪(燕山晚期)为造山期后大规模伸展垮塌作用与伸展盆地的发育阶段；新生代(喜山期)为远距离碰撞效应与弱挤压挠曲性质的稳定大陆内坳陷的发育阶段。
In the northern part , the oceanic crust occurring between the bayan har and kunlun terranes started subduction from south to north at about 243 ma , and did not stop until the development of post - orogenic pog - type granite in the bayan har terrane at 220 ma , thus illustrating the orogeny in the form of subduction and collision kept active for over 20 ma 以pog型花岗岩在巴颜喀拉地体内大量生成、在阿尼玛卿岩带中较多出现、在昆仑岩带利金沙江岩带少量出现为标志。期： 160 - 140ma ，断裂系活动；金沙江、东昆仑剪切作用发生；部分岩体动力变质变形。
