摘要
尾亚韧性剪切带形成于石炭纪晚期。根据其宏观变形构造、显微变形构造等变形特征 ,说明其经历了早期的推覆剪切和后期的右行推覆剪切两个主要演化阶段。
The Weiya ductile shear zone formed in the last stage of Carboniferous Period.According to its macroscopic and microscopic deformation structures,it at least went through two main stages of evolution from the thrusting nappe shearing to dextral nappe shearing. This adds some new contents to researching the history of the structure evolution in the region as well as directing to find deposits.
出处
《西安工程学院学报》
2001年第4期28-31,40,共5页
Journal of Xi'an Engineering University
