广东大地构造位于华南加里东地槽褶皱系。
Tectonically, Guangdong is located in the south China Caledonian Geosynclinal Folded System.
该区金直接来源于加里东和华力西花岗岩。
晚加里东-海西期花岗岩侵入体与金矿密切相关；
The formation of gold mine is closely related to the intrusive bodys of granite, which are formed between later Caledonian and Hercynian.
羊露河上游铁矿位于北祁连西段加里东褶皱带西段。
Iron ore deposits in upper reach of Yangluhe river are situated in the west Calidonian fold belt of the west Qilianshan mountain.
着重分析了加里东早期张性正断裂的平面和剖面特征。
The paper focus on the horizontal and vertical characters of tensional normal fault formed in the early Caledonian.
山体岩石为加里东期花岗岩和大理石，距今4——6亿年。
Rock Hill Caledonian granite and marble ago 4-6 billion years.
加里东运动以后，扬子和华夏陆块拼合成统一的华南板块。
After the Caledonian orogeny, the Yangtze plate and the Cathaysia landmass were matched together to be the united plate of south China.
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 area was wholly uplifted with caledonian orogeny in the early palaeozoic , and underwent thereafter denudation.
关陵根铅锌矿床位于西秦岭北带关子镇—太阳寺加里东构造带上。
Guanlinggeng Pb-Zn mine is located at Caledonian tectonic zone in Guanzi Township and Taiyangsi area of northern belt of west Qinling.
下古生界在加里东运动暴露期间，黔中隆起及周缘盖层化学损失量巨大。
The loss amount of caprocks was huge because of the exposure and chemical erosion during the Caledonian tectonic movements around the upheaval in the middle of Yunnan province.
该类型构造形成于加里东期末，是该区加里东造山期后隆升背景的产物。
This kind of structure is the product under background of the uplift in Caledonian postorogenic phase formed at the end of the Caledonian Stage.
香港地区届华南加里东构造—岩相带南缘，中生代西太平洋岩浆活动带一部分。
Hong Kong special district, located in the south margin of Caledonian tectonic-lithofacies belt, belongs to the part of west Pacific magmatic mobile belt of Mesozoic.
统一陆壳也是显生宙以来逐步形成的：主要经历了加里东和华里西-印支两大构造阶段。
The Qinghai crust was gradually collaged during the Paleozoic and mainly underwent Caledonian and Hercynian-Indosinian tectonic events.
加里东期断裂控制了加里东岩溶储层的发育，由此预测了加里东期岩溶储层的发育区带。
Based on the domination of Caledonian faults on the development of Caledonian karst reservoirs, this paper predicts the development area of Caledonian karst reservoirs.
华南的大地构造有两种解释，一种可称为加里东造山模式，另一种可称为华南阿尔卑斯模式。
There are two tectonic interpretations of South China tectonics, of which one can be called "Caledonian model" and another called "South China Alps model".
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
上扬子区在加里东运动过程中形成前陆盆地，主要经历了三次挤压、挠曲沉降至松驰、抬升过程。
The tectonic subsidence is the main controlling factor in the foreland basin, which went through three periods, namely press, flexure subsidence to laxitas, uplift.
这些发现为研究本区加里东期的大地构造环境和变形特点、扬子板块与华南板块的相互作用提供了新资料。
These findings provide new information for the study of the Caledonian tectonic setting and deformation features in the area and the interaction between the Yangtze and South China plates.
闽西北中元古代地层在加里东运动期间遭受了变形变质作用，形成了一套片岩—片麻岩—混合岩系变质岩。
The Middle Proterozoic group Strata in northwest Fujian had been Subjected metamorphism in Caledonian orogeny, and formed a metamorphic rock association of schist-gneiss-migmatite series.
加里东中期奥陶系碳酸盐岩古岩溶储层作为未来塔河油田重要的勘探领域，有助于今后该油田的油气勘探。
Since the middle Caledonian karst reservoir is an important region for future exploration in the Tahe oilfield, it is believed to be a great help for petroleum exploration.
加里东期在东秦岭—大别造山带南侧江汉平原地区存在一个继承性古隆起，前人所称的“鄂中古陆”是其具体的表现。
There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.
研究区主要发育加里东期—海西期近EW、NE向、NW向断裂，为油气运移提供良好的通道，同时控制着圈闭的形成与发育。
The faults in work area are mainly in EW, NE, NW and formed during Caledonian-Hercynian, offering favorable channels for petroleum's migration and controlling the formation and growth of traps.
该区经历了六个构造形变期，以相当于 主加里东期的第二期（D_2）与喜马拉雅期的第五期（D_5） 形变期最为重要。
The area has undergone six stages of tectonic deformation with the second episode of Caledonian Movement (D_2) and the fifth episode of Himalayan Movement (D_5) as the most important ones.
区内下古生界烃源岩经历了两次成油过程，第一次发生在加里东运动前的盆地沉降阶段，第二次发生在加里东运动后晚古生代陆表海沉积阶段。
The first was in the basin subsidence stage that was prior to the Caledonian movement. The second took place in the marginal sea deposition stage after the Caledonian movement.
区内下古生界烃源岩经历了两次成油过程，第一次发生在加里东运动前的盆地沉降阶段，第二次发生在加里东运动后晚古生代陆表海沉积阶段。
The first was in the basin subsidence stage that was prior to the Caledonian movement. The second took place in the marginal sea deposition stage after the Caledonian movement.
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