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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

黄俊 鲁如魁 褚志安 张永强

中国地质2011,Vol.38Issue(3):544-552,9.
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

黄俊 1鲁如魁 1褚志安 2张永强3

作者信息

  • 1. 安徽省地质调查院,安徽合肥230001
  • 2. 西北大学地质学系,大陆动力学国家重点实验室,陕西西安710069
  • 3. 陕西地勘局第六地质队,陕西临潼710060
  • 折叠

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. ()

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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