• 责任者：Yang Wangtun (College of Earth Sciences and Resources ; Chang’an University ; Xi’an 710054 ; China) ; Duan Lizhi
• 刊名：Northwestern Geology
• 出版年：2013
• 卷期：46(2)
• 关键词：韧性剪切带 ; ductile shear zones ; 甘肃 ; Gansu Province
• 页码：p.44-53
• 图表：11 illus., 1 table, 29 refs.
• 分类号：0300
• issnNo：ISSN1009-6248
• isbnNo：CN61-1149/P

     The kinematic and dynamic characteristics of Longshoushan ductile shear zone in the early period of Caledonian orogeny was mainly the bottom-up tensile stress. In the middle period, it was largely dextral pure shearing action which was NW-SE trend. In the last period, it was the positive pressure of NE-SW trend accompanied by local press twist action. According to the distribution of the ductile shear zone in the strata, namely only in Jixianian System and Sinian System, the authors conclude that the ductile shear zone should be formed after Sinian Period. Combined with the age of Jinchuan ultrabasic complex, we can conclude that the ductile shear zone has no contribution to Jinchuan deposit, but maybe it can help the ultrabasic complex move to shallow zone.