绿片岩（green schist）又称绿色片岩，是绿色至暗绿色具细粒鳞片变晶结构，千枚状至片状构造的区域变质岩石的统称，是片岩的一种。
... 黑云康煌岩 biotite camptonite 黑云绿泥亚相;绿片岩 biotite chlorite subfacies(green schist) 黑云母 biotite ...
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绿片岩 biotite chlorite subfacies(green schist); gree chist; green-schist 蓝片岩相 蓝闪片岩相 blueschistfacies .
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绿片岩 biotite chlorite subfacies(green schist); gree chist; green-schist 蓝片岩相 蓝闪片岩相 blueschistfacies ..
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绿片岩相 greenschist facies ; green schist facies
又称高压绿片岩相 high pressure greenschist facies
蓝闪石-绿片岩相 glaucophane-greenschist facies
阳起石绿片岩相 actinolitegreenschist facies
硬绿泥片岩 [岩] chloritoid schist ; ottrelite-schist ; chloritoidschist
蓝闪绿片岩相 glaucophane greenschist facies
斜长阳起绿片岩 chlorogrisonite
绿泥闪帘片岩 prasinite
阳起绿色片岩相 actinolitic greenschist facies ; actinoliticgree chistfacies
Besides a suit of greenschists, in which hornblende schist is in majority, is discoveredalso in this area. Research shows that the greenschist is metamorphosed from N-MORB.
此外考察中还发现一套以角闪片岩为代表的绿片岩，经研究是由N-MORB变质而来的。
参考来源 - 吉林省延边开山屯地区蛇绿混杂岩·2,447,543篇论文数据，部分数据来源于NoteExpress
绿片岩原岩是一套含板内拉斑玄武岩的火山沉积建造。
The greenschists originated from a series of volcanic - sedimentary formations with intercalated intracontinental tholeiites.
川西高原广泛分布的西康群，原视为区域低温动力变质作用低绿片岩相变质岩。
Xikang Group is widely exposed on the West Sichuan Plateau and was considered to be a low greenschist facies metamorphic rock due to regional low-temperature dynamometamorphism.
变质相由基底岩系的低角闪岩相—高绿片岩相逐渐过渡为上覆盖层的低绿片岩相。
The metamorphic facies gradually change from low amphibolite—high green-schist facies of the basement to low green-schist of the cover.
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