内蒙古苏尼特左旗韧性剪切带研究  

STUDY OF SUNITZUOQI DUCTILE SHEAR ZONE IN INNER-MONGOLIA

作　　者：高德臻[1] 徐有华 

机构地区：[1]中国地质大学,北京100083 [2]赣州南方工业学校,赣州341000

出　　处：《地质与勘探》2000年第5期31-35,共5页Geology and Exploration

摘　　要：通过对韧性剪切带的研究 ,认为 :这些韧性剪切带形成于印支运动 ,与中朝板块和西伯利亚板块在早二叠世末对接碰撞造山有成生联系。Sunitzuoqi locates in the middle part of the northern margin of Sino-Korea region. Bayanwundur-Wlainaobao ductile shear zone is the typical one in them. This ductile shear zone were formed in the stage of Indosinian movement. The formation of the ductile shear zones in this region are related to the collision and the orogeny between the Sino-Korean and Siberian plates during the end of the early Permian.

关 键 词：苏尼特左旗 韧性剪切带 印支运动 

分 类 号：P542.3[天文地球—构造地质学]