中国地质Issue(4)：1205-1214,10.
内蒙古苏布格塔蓝闪石片岩基本特征及成因分析
Basic characteristics and genetic analysis of glaucophane schist in Subugeta, Inner Mongolia
摘要
Abstract
The studied glaucophane schist is in the Ordovician Halahahe Formation of Subugeta, Inner Mongolia, and there are a variety of rock assemblage types. According to the optical characteristics and EMP analysis, the authors have come to the conclusion that the glaucophane schist is a kind of ferriglaucophane in the study area. The topomineral assemblage of glaucophane schist is characterized by glaucophane + epidote + actinolite + phengite + sphene. The schist was cemented and recrystallized by shaly clasolite, and the formation environment of native rock was the marginal-sea basin of the continent. The metamorphic origin belonged to the regional low-temperature/middle-high pressure dynamic metamorphism related to plate movement.关键词
蓝闪石片岩/电子探针/标型矿物组合/边缘海盆地/板块运动Key words
glaucophane schist/EMP/topomineral assemblage/marginal-sea basin/plate movement分类
天文与地球科学引用本文复制引用
张庆奎,邵学峰,关培彦,杨宾,赵明远,李安楠,吕凤祥..内蒙古苏布格塔蓝闪石片岩基本特征及成因分析[J].中国地质,2014,(4):1205-1214,10.基金项目
中国地质调查局地质调查项目(1212011120668)资助。 （1212011120668）
