中国地质2011,Vol.38Issue(3):544-552,9.
内蒙古察右后旗三道沟一带韧性剪切带磁组构特征及其构造意义
Magnetic fabric features of the ductile shear zone in Sandaogou area of Inner Mongolia and their tectonic significance
摘要
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.关键词
磁组构/三道沟韧性剪切带/临河-集宁断裂Key words
magnetic fabrics/Sandaogou ductile shear zone/Linhe-Jining fault分类
天文与地球科学引用本文复制引用
黄俊,鲁如魁,褚志安,张永强..内蒙古察右后旗三道沟一带韧性剪切带磁组构特征及其构造意义[J].中国地质,2011,38(3):544-552,9.基金项目
内蒙古自治区地质勘查项目"1:5万内蒙古自治区察右后旗袁家房子等四幅矿产地质调查"资助. ()