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这个时期是全面的上升和造山运动。The period was one of general emergence and orogeny.

前陆盆地是研究造山运动的关键地区之一。Foreland basins are the key areas for the study of orogeny.

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铁堡运动是作者1960年于山西工作时首先发现和命名的。The Tiebao Orogeny was first discovered and named by the author in 1960.

碰撞造山作用是一个在碰撞事件之后的均变过程。The collision orogeny is a uniformitive process after the collision event.

而区域性的南-北向构造实质是海西运动前构造形迹的残留。The regional S-N trench tectonics is actually heritages before Hercynian orogeny.

伴随着造山运动的地壳运动出发了一场广泛的火成活动。The earth movements associated with the orogeny triggered an extensive igneous activity.

人工造山在中国传统造园中便自然占有十分突出的地位。Artificial orogeny in traditional Chinese garden occupies a very prominent position and natural.

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前陆盆地的终结标志着碰撞造山作用的结束。The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny.

是开展陆内造山和再生造山研究的理想之地。The Bogda mountain chain is an ideal area for the study of intracontinental orogeny and revival orogeny.

庐山-彭山地区原是一个经受印支早期伸展机制下所形成的变质核。Lushan-Pengshan region was a metamorphic core formed by tensional regimes in the early Indosinian 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。Since the Permian, the Tarim Basin had undergone basinal extension, subduction and intro-continental orogeny.

大巴山前陆构造是后秦岭造山运动的陆内造山的结果。The foreland of Daba Mountains resulted from the intracontinental orogeny of the Qingling orogenetic movements.

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板缘造山主要表现为岩石圈和软流圈以基本相同的运动趋势的相对运动。Maginal orogeny was formed on this condition with same relative motion trend between lithosphere and asthenosphere.

相邻造山带时空上不均一的造山作用对盆地的影响不同,形成了盆地独特的结构。The inhomogenous orogeny in time and space of the adjacent orogenic belts forms the peculiar structure of the basin.

小秦岭石英脉型金矿主要产在华山、文峪等中生代花岗岩基南侧的太古宙荡泽河群绿岩带和早元古代滴沟群孔达岩系中。It is a hypergene, medium-low temperature quartz vein type gold deposit located in the granite of the early Variscan 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。Therefore, the petrochemical data provide the P-T conditions of crustal melting in the peak period of the Yanshanian orogeny.

结果秦岭造山带存在加里东期、印支期和燕山期的几个关键成矿地质事件。Results There are the key metallogenetic events during the Caledonian, Indosinan and Yanshanian periods in the Qinling Orogeny.

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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。The unconformity between the basement and the cover is the record of Wuling orogeny equal to Luliang orogeny of Huabei platform.

板内造山主要表现为同一区域内岩石圈、流圈等不同层圈之间的不协调的相对运动。Whereas the intraplate orogeny show that an inharmonious relative motion between different spheres was happened in the same region.

新生代随着印度板块同欧亚大陆的碰撞,开始隆升。Intra-continental orogeny was initiated since Late Permian, and uplift occurred during the Cenozoic due to Indian-Eurasian collision.