加里东运动

加里东运动主要为近SN向的挤压褶皱作用，此时断裂带可能形成了构造薄弱带；

Near SN compressive folding occured in Caledonian orogeny , and at this time this fault zone maybe an unsubstantial tectonic belt ;

东秦岭古洋盆与加里东运动

The ancient ocean and Caledonian orogeny in the East Qinling

论下扬子-钱塘地区晚加里东运动

On late - Caledonian movement in lower Yangtze - Qiantang region

这是广西加里东运动的主幕。

This was the main phase of the Caledonian Movement in Guangxi .

贵州加里东运动的地层学效应

The Stratigraphic Effect of the Caledonian Movement in Guizhou

华南加里东运动演化过程中烃源岩的成生

The formation of hydrocarbon resources during the evolution of South China in Caledonian

早加里东运动，造成下早奥陶统与寒武系的假整合；

The Early Caledonian movement resulted in a pseudo-conformity between Cambrian and Lower Ordovician .

浙西的加里东运动

The Caledonian movement in western part of Zhejiang

D4期变形为后期加里东运动的产物。

The deformation D4 resulted from Caledonian movement .

赋矿层位为加里东运动后第一个海浸沉积序列的碎屑岩向碳酸岩的过渡相，岩相古地理环境控制作用明显。

It occurs in the transitional horizon from Caledonian movement and is controlled by lithofacies and palaeography .

自加里东运动以来，它长期屎持相对坳陷或低地特点。

It has always maintained the character of the relative depression or low land since the Caledonian movement .

试论中国地台南部加里东运动的影响及其大地构造发展史

Remarks on the effect of the Caledonian movement and geotectonic history on the southern part of the Chinese platform

加里东运动期间的构造抬升和拆离是造成该区变质作用温度-压力差异的主要原因。

The tectonic uplift and sliding in Caledonian orogeny is the main cause of causing the metamorphic temperature and Pressure difference in this area .

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 .

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 .

区内下古生界烃源岩经历了两次成油过程，第一次在加里东运动前的盆地沉降阶段，第二次在加里东运动后晚古生代陆表海沉积阶段。

The Lower Paleozoic source rock in the region has undergone two oil generation processes , the first one has taken place in basin subsidence before Caledonian movement .

构成这一特殊沉积格局的主要原因是该区沉积相受加里东运动期间形成的基底断裂控制。

The major cause leading to such a distribution pattern is that the sedimentary facies in this district was controlled by the foundation faults formed in Caledonian orogeny .

中国古大陆沉积-构造演化在加里东运动期和海西-早印支运动期，发育两个构造层次的海相盆地。

Two structural strata of the marine basins are developed in Caledonian movement and Hercynian-early Indo-China movement for Chi - na 's old land sedimentary and tectonic evolutions .

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 .

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 .

加里东运动使华南褶皱带与扬子地台南缘拼贴，形成广阔而稳定的后加里东地台；

The south margin of the Lower Yangtze Platform linked with the South China Folded Belt during the Caledonian Movement , and the stable and wide Post-Caledonian Platform was formed .

大约408Ma左右结束的加里东运动使包括广西在内的整个中国南方隆升为陆，为泥盆纪沉积盆地的形成奠定了基础。

Caledonian orogeny , ending at about 408 Ma , made the whole southern China including Guangxi upheave to be continent and laid a base for the formation of Devonian basins .

加里东运动在盆地南部和秦岭北部造成的一系列构造现象显示，秦岭北部加里东期造山作用对盆地晚古生代沉积起到一定的控制作用。

A lot of structure phenomenon was caused by Caledonian movements in southern basin and North-Qinling , which showing the sedimentary process was controlled by the orogenesis of north-Qinling in Caledonian .

加里东运动形成于奥陶纪晚期，可再细分为两期，分别与北秦岭构造带早古生代的弧－陆碰撞与陆－陆碰撞作用有关。

The Caledonian movement took place in late Ordovician and may be divided into two phases , corresponding to arc-continent collision and continent-continent collision in the North Qinling orogenic belt during early Paleozoic Era respectively .

属于被动大陆边缘裂谷盆地的滇黔桂盆地，自加里东运动之后，泥盆纪开始拉开，整个晚古生代延续发展。

The Yunnan-Guizhou-Guangxi basin is a passive continental-margin rift basin . After the Caledonian movement , it began to be pulled apart in the Devonian and continued to develop in the whole of the Late Paleozoic .

其中，前三期构造变形作用发生于晋宁期，第四期构造变形作用为后期加里东运动叠加的产物，四期构造变形作用所形成的构造形迹各不相同。

The first three episodes took place in the Jinning epoch and the last episode occurred in the later period of the Caledonian movement . The structural features formed by four episodes of structural deformations are quite different eath other .

根据区域不整合关系，变质和变形构造特征，进一步确定了加里东运动是海南岛地壳演化历程中一次极其重要的造山事件，区域上与华南地区晚加里东运动进行对比。

According to the regional angular unconformity and metamorphic and deformational characteristics , the Caledonian movement has been determined to be an important tectonic event in the crustal evolution of Hainan Island and may be compared with the Late Caledonian movement of South China .

由于加里东运动的影响和同沉积断裂的控制，狭窄的斜坡相格局从中泥盆世-早石炭世早期都特征明显，相带的迁移伴随断裂的改变而改变。

Finally it developed into carbonate ramp because of settlement or changes of sea level.4.As the impact of the Caledonian movement and control of syndepositional faults , the phase pattern characters of the narrow slope from Devonian to Early Carboniferous are obvious . Phase belt migration followed with changed faults .

它们表明加里东构造运动的早期对浙江龙泉地区产生了重要影响。

The early Caledonian tectonic movement has exerted significant influence on the studied district .

这些新的高精度年龄学数据为武夷山加里东构造运动时限和性质提供了精确约束。

These high precision dating date provide constrains on the timing and nature of the Caledonian Movement in the Wuyi Mountains .