摘要
研究了桐柏地区新城—应山韧性剪切带的变形特征、动力学成因机制，并根据横切韧性剪切带的３条剖面的变形特征，认为中生代华北、扬子两大板块陆陆碰撞的动力来自扬子板块。
he deformation features and genetic dynamic mechanism of Xincheng Yingshan ductile shear zone in Tongbai area are studied in this paper. From the deformation features of the ductile shear zone, the authors think that the dynamics of the collusion between the North China Plate and the Yangtze Plate in the Mesozoic is from the Yangtze Plate.
出处
《现代地质》
CAS
CSCD
北大核心
1998年第2期194-196,共3页
Geoscience
关键词
韧性剪切带
应变测量
陆-陆碰撞
桐柏地区
ductile shear zone, deformation measurement, inter land collusion
