石英片岩（quartz schist）是一种含石英较多的具片状构造的区域变质岩石。主要由石英、酸性斜长石、绢云母、绿泥石或白云母、黑云母等组成，其中石英和长石的含量大于50%（长石含量小于25%）。
Zhalantong Group was identified and named in 1976 during 1 : 200000 geologic survey in Buteha-qi. It is consisted of chlorite-quartz schist, crystalline limestone and hematite-quartz.
扎兰屯群创名于1976年1∶20万布特哈旗幅区域地质调查报告，是一套由绿泥石英片岩、结晶灰岩及赤铁石英岩组成的区域变质地层，自下而上划分为刘家崴子组、城基嘎查组和郝家沟组。
参考来源 - 大兴安岭北部扎兰屯群的解体及构造意义探讨·2,447,543篇论文数据，部分数据来源于NoteExpress
主要岩石类型为二云石英片岩和斜长角闪片岩。
The main rock types are two-mica quartz schist and plagioclase amphibole schist.
大别山北部佛子岭群变碎屑岩主要由板岩、千枚岩和云母石英片岩等所组成。
Foziling Group in the Dabie Mountains is composed of SLATE, phyllite, mica quartz schist, etc.
驼路沟钴、金矿位于东昆仑褶皱系昆南断褶带内，产于晚古生代二叠系下统石英片岩中。
Tuoluogou cobalt and gold deposit is in the south of the east Kunlun drape. It formed in quartz schist in the forepant Permian of late vecent life.
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