1) Caledonian movement
加里东运动
1.
Zircon La-ICPMS U-Pb Dating of the Weipu Granitic Pluton in Southwest Fujian and the Changpu Migmatite in South Jiangxi:Constrains to the Timing of Caledonian Movement in Wuyi Mountains
闽西南玮埔岩体和赣南菖蒲混合岩锆石La-ICPMS U-Pb年代学:对武夷山加里东运动时代的制约
2.
It is noted that the distinct function of Caledonian movement in this area is the formation of the linear migmatization and granitization on the basis of rift and tumescence basement.
本文提出武夷及其邻区存在两个裂陷槽及一裂隆，鹰潭－南城－安远－河源韧性断裂带为东部的火山岩型与西部的花岗岩型铀矿床的地质分界线，指出了加里东运动在本区的突出作用是使裂隆基底岩石发生混合花岗岩化作用。
3.
Through 1∶250000 regional geological mapping, many Caledonian tectonic deformation features and unconformable contact relationships at several sites were found in Sinian-Lower Paleozoic strata, indicating that Caledonian movement was strong in this area and that the Ca.
通过1∶25万区域地质填图,在震旦纪—下古生代地层中发现大量加里东期构造变形形迹和数处不整合接触关系,表明本区加里东运动强烈,华南地区广泛发育的加里东运动已经强烈地影响到扬子板块的南缘。
2) Caledonian orogeny
加里东运动
1.
9Ma,indicating the Yanwan intrusions formed at the end period of Late-Silurian and are the products of Caledonian orogeny in the late Paleozoic.
9Ma,属末志留世晚期,该侵入体应是早古生代晚期加里东运动碰撞造山过程的产物,其形成时代(414。
3) Caledonian tectonic movement
加里东构造运动
5) Caledonian orogeny
加里东造山运动<地>
6) THE CALEDONIAN MOVEMENT IN WESTERN PART OF ZHEJIANG
浙西的加里东运动
补充资料：加里东运动
加里东运动 古生代早期地壳运动的总称。
其所形成的褶皱带称加里东褶皱带。1888年由休斯（e.suess）创用，主要指欧洲西北部晚志留纪至泥盆纪形成北东向山地的褶皱运动。这一时期的地壳运动，使延伸于北爱尔兰、苏格兰和斯堪的纳维亚半岛的北东向格兰扁地槽、西伯利亚的萨彦岭地槽、中国东南部加里东地槽、澳大利亚的塔斯马尼亚地槽及北阿帕拉契亚地槽（古大西洋）形成褶皱山地。加里东运动的完成标志着早古生代的结束。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条