摘要
本文首次报导了在宿松地区经多种测试查证，有经受高压变质作用的黄玉、天蓝石，及石榴子石、角闪石、蓝晶石中柯石英的存在，并将以黄玉为标志的富铝泥质岩（Ｓｃｈｒｅｙｅｒ称其为广义白片岩），参照蓝片岩、绿片岩的命名原则，易名为黄片岩。深入的矿物学研究表明本区是一条有充分矿物学依据的超高压变质带。
The paper on basis of identification of many tests first reports the existence of high─Pmetamorphic topaz,lazulite l garnet,hornblende and coesite in the Susong area. The aluminum─rich argillite(broadly called white schist by Schreger) marked with topaz is renamed yellow schist by reference to the nomenclature of blue schist and green schist.Study indicates that the Susong area is a ultra─high pressure metamorphic belt with enough mineralogical evidences.
出处
《安徽地质》
1995年第3期66-69,共4页
Geology of Anhui
关键词
超高压变质带
天蓝石
黄玉
柯石英
黄片岩
ultra─hish─P metamorphic belt,lazulite,topaz,coesite,yellow schist.
