约100年前,C.Lapworth 描述了苏格兰高地莫伊内冲断层带埃里波尔的一种页理发育的细粒岩石,并取名为糜棱岩。从那以来,地质学家们已经认识到,糜棱岩指示集中变形带,包括大陆规模的集中变形带。近年来,一些方面的进展,包括用来研究细粒岩石的透射电子显微镜和化学显微分析技术,以及 About 100 years ago, C. Lapworth described a finely-grained, finely-grained rock called the Eriebole in the Moine fault zone of the Scottish Highlands and named it mylonite. Since then, geologists have realized that mylonites indicate a concentrated deformation zone, including a concentrated deformation zone on a continental scale. In recent years, some advances have included transmission electron microscopy and chemical microanalysis techniques used to study fine-grained rocks, as well as