【摘要】 变形岩石的磁组构参数K1、K2、K3、P、T、F、L、E等可以用来定量地分析和了解构造变形的性状。笔者对分布于察哈尔右翼后旗三道沟一带的构造岩进行磁组构特征研究发现:E值多大于1,或接近于1;T值大于0的明显多于小于0的;P值均大于1,而以F和L的对数值为轴所作的变型弗林图解中数据主要集中在剪切区和压扁区。上述结果表明磁化率椭球体主要表现为磁面理较磁线理发育的压扁型椭球体,三道沟一带韧性剪切带的构造岩石经历了力学机制为挤压剪切的强烈构造活动。这种由磁组构揭示的应力应变特征得到了野外露头及显微构造的佐证。更多还原

【Abstract】 The parameters of magnetic fabrics of deformed rocks such as Kmax,Kint,Kmin,P,T,F,L and E can be used to quantitatively display the behaviors of tectonic deformation.Characteristics of magnetic fabrics of the ductile shear zone in Sandaogou area of Inner Mongolia were analyzed in this study.The results show that most E values are larger than or close to 1;T values larger than 0 are more than those smaller than 0;P values are larger than 1,and the data in graphic variant Flinn of the L-F parameters of magnetic fabrics are concentrated in the shear zone and the compression zone.It is indicated that the magnetic susceptibility ellipsoid mainly finds expression in flatted ball ellipsoid whose foliation is more developed than lineation.The rocks in Sandaogou ductile shear zone experienced a strong tectonic activity of extrusion shear mechanical mechanism.The stress,strain and deformation characteristics are consistent with field features and microstructure.更多还原