加里东运动是古生代早期地壳运动的总称。泛指早古生代寒武纪与志留纪之间发生的地壳运动，属早古生代的主造山幕。欧洲普遍用于早古生代变形的名词。以英国苏格兰的加里东山而命名，志留系及更早地层被强烈褶皱，与上覆泥盆系呈明显的不整合接触。形成从爱尔兰、苏格兰延伸到斯堪的纳维亚半岛的加里东造山带。
...南及邻区加里东运动的表现及地质意义 关键词：加里东运动；地质意义；黔东南及邻区 [gap=1803]Key words：Caledonian Movement；geological significance；southeastern Guizhou and its adjacent area ...
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加里东运动（Caledonian orogeny）+ r7 `1 {) p2 y3 | 泛指早古生代志留纪与泥盆纪之间发生的地壳运动,属早古生代的主造山幕。
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... 钙白云石 caledolomite 加里东运动 Caledonian fold(ing) 加里东运动 Caledonian movement ...
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加里东造山运动 Caledonian mountain-building movement
加里东宁造山运动 Caledonian orogeny
后加里东造山运动复活 Post caledonian regeneration
加里东构造运动 Caledonian tectonic movement
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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.
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.
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