大王山岩体南缘糜棱岩带磁性组构  

MAGNETISM FABRIC OF DAWANG MOUNTAIN ROCK MASSES MYLONITE ON SOUTHERN EDGE

作　　者：潘明宝 

机构地区：[1]江苏地矿局区调队

出　　处：《华东地质学院学报》1993年第1期50-55,64,共7页Journal of East China Geological Institute

摘　　要：本文采用岩石磁化率各向异性的测量方法,对大王山南缘糜棱岩带磁性组构进行研究;提供了岩石变形性质,反映了矿物在变形过程中的行为,其优点是快速和综合性强。This paper studies the magnetism fabric of Dawang Mt. mylonite on. southern edge with the method of anisotropy survey of petrological susceptibility. It not only gives petrology deformation property, but also indicates the behavior of minerals in the process of deformation. The advantages of it are: it is of fast speed and good synthetical property.

关 键 词：糜棱岩 磁化率 磁性组构 岩体 

分 类 号：P318.4[天文地球—固体地球物理学]