Foreland basins are the key areas for the study of orogeny.
前陆盆地是研究造山运动的关键地区之一。
In late Himalnyan orogeny, it mainly show regional elevation.
喜山晚期运动主要为区域抬升作用。
Orogeny stands for mobile stages in the evolution of the crust.
造山运动是地壳演化活动阶段的反映。
The Tiebao Orogeny was first discovered and named by the author in 1960.
铁堡运动是作者1960年于山西工作时首先发现和命名的。
The collision orogeny is a uniformitive process after the collision event.
碰撞造山作用是一个在碰撞事件之后的均变过程。
In the late Yanshan orogeny, this area was characterized by brittle fracture.
燕山晚期本区以脆性构造为主，断裂构造发育。
A velocity variation boundary belt appears beneath the Dabie-Sulu orogeny belt.
大别-苏鲁造山构造带下面存在着一条地震波速度变化带。
The general setting of Tarim basin was shown in compression at Late Hercynian orogeny.
海西晚期，塔里木板块总体为挤压背景。
Near NW-SE compressive folding occurred in early Yanshan orogeny, when it began to buckle.
燕山早期运动主要为NW-SE向的挤压褶皱作用，断裂带走向开始弯曲变形；
The effective traps for petroleum accumulation were developed mainly in late Yanshan orogeny.
燕山晚期运动为本区的油气聚集提供了有效的圈闭。
Artificial orogeny in traditional Chinese garden occupies a very prominent position and natural.
人工造山在中国传统造园中便自然占有十分突出的地位。
These different cooling histories may reflect the differential uplifting of Qinling orogeny belt.
这种不同的冷却历史可能反映了东、西秦岭的差异隆升过程。
The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny .
前陆盆地的终结标志着碰撞造山作用的结束。
The first part of this paper briefly introduces various main concepts of orogeny and basin formation.
本文第一部分简述了多种主要造山理论和成盆学说；
The Altai orogeny, as one of notable crustal accretion areas, is famous for its abundant mineral deposits.
阿尔泰造山带是中亚地区显生宙大陆地壳增生明显的地区之一，蕴藏丰富的矿产资源。
Since the Permian, the Tarim Basin had undergone basinal extension, subduction and intro-continental orogeny.
塔里木盆地自二叠纪以来，历经盆地扩张和盆地俯冲以及陆内造山作用的过程。
The foreland of Daba Mountains resulted from the intracontinental orogeny of the Qingling orogenetic movements.
大巴山前陆构造是后秦岭造山运动的陆内造山的结果。
The area was wholly uplifted with caledonian orogeny in the early palaeozoic , and underwent thereafter denudation.
早古生代以来，加里东运动使本区全面上升，同时遭受剥蚀。
The effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed.
分析了燕山运动和喜马拉雅运动在准噶尔盆地油气运移和聚集中的作用。
Therefore, the petrochemical data provide the P-T conditions of crustal melting in the peak period of the Yanshanian orogeny.
所以，这些强过铝质侵入岩的岩石化学数据提供了关于燕山运动峰期地壳发生部分熔融时的温压条件的信息。
The unconformity between the basement and the cover is the record of Wuling orogeny equal to Luliang orogeny of Huabei platform.
基底与盖层之间的高角度不整合界面，系武陵造山运动的记录。武陵运动与华北地台的吕梁运动相当。
After the Caledonian orogeny, the Yangtze plate and the Cathaysia landmass were matched together to be the united plate of south China.
加里东运动以后，扬子和华夏陆块拼合成统一的华南板块。
Velocity values beneath Sulu region and the Shandong peninsula are in the identical contour line with that beneath the Dabie orogeny belt.
苏鲁、山东半岛下面的速度分布与大别造山带下面的速度分布处于同一个速度等值区域上。
The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
班公湖-怒江带以北，表现为强烈的造山运动，形成规模巨大的印支造山带。
These evidences provide forceful support for tectonic interpretation of the Triassic orogeny and the tectonic evolution model in South China.
这些证据为华南的三叠纪造山作用和构造演化模式提供了强有力的支持。
As a typical orogeny of continental collision, Qingling has no condition for large scale UHPM formation, although scattered UHPM may not be excluded.
秦岭作为典型造山带，虽然不排除零星超高压变质的可能，但不具备大规模超高压变质的条件。
Regional very low grade metamorphism resulted from the combination of early diagenesis burial metamorphism (pre orogeny) and late syn orogeny metamorphism.
并指出区域极低级变质作用是成岩-埋藏变质作用(造山前)和同造山变质作用的综合结果。
Based on modern tectonic theory, the authors believe that this conglomerate is a product of middle-late stage sedimentation during a compressional orogeny.
本文根据现代构造理论，认为修水组底部砾岩属于挤压造山作用中晚期的沉积产物。
Based on modern tectonic theory, the authors believe that this conglomerate is a product of middle-late stage sedimentation during a compressional orogeny.
本文根据现代构造理论，认为修水组底部砾岩属于挤压造山作用中晚期的沉积产物。
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