| 华北与扬子板块碰撞带青岛仰口构造混杂岩的三期变形及区域构造意义 |
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| 引用本文： | 刘德良,李曙光,葛宁洁,张志敏,王来明,韩宗珠,赵广涛.华北与扬子板块碰撞带青岛仰口构造混杂岩的三期变形及区域构造意义[J].中国科学技术大学学报,1994(3). |
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| 作者姓名： | 刘德良 李曙光 葛宁洁 张志敏 王来明 韩宗珠 赵广涛 |
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| 作者单位： | 中国科技大学，山东省区域地质调查队，青岛海洋大学 |
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| 摘 要： | 青岛仰口构造混杂岩位于大别－胶南造山带东段，为华北与扬子板块碰撞带边界韧性剪切带内的蛇绿混杂岩．它大体经历了三期变形，始于印支期，历经燕山期至后燕山期．
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| 关 键 词： | 多期变形，构造混杂岩，板块碰撞带，青岛 |
The Three Epoch Deformations and Tectonic Significane of the Qingdao Yangkou Tectonic Melange in the Collision Zone of the North China Plate and the Yangtze Plate |
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| Liu Deliang,Li Shuguang,Ge Ningjie.The Three Epoch Deformations and Tectonic Significane of the Qingdao Yangkou Tectonic Melange in the Collision Zone of the North China Plate and the Yangtze Plate[J].Journal of University of Science and Technology of China,1994(3). |
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| Authors: | Liu Deliang Li Shuguang Ge Ningjie |
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| Institution: | Liu Deliang;Li Shuguang;Ge Ningjie(University of science and Technology of Chian)Zhang Zhimin;Wang Laiming(Regional Geological Reconnaissance Institute of Shandong)Han Zongzhu; Zhao Guangtao(Qingdao Ocean Universiyh) |
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| Abstract: | The Qingdao Yangkou tectonic melange lies in the east of Dabie Mountain-South Shandong Orogenic Zone,and belongs to a ophiolite melange in the huge ductile shear zone of the collision zone between the North China Plate and the Yangtze Plate. It has undergone three epoch tectonic deformations in indosinian Period,Yanshan Period and Hymalayan Period. |
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| Keywords: | multiple deformation tectonic melange plate collision zone Qingdo |
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