1) Basic rock-type granulite
基性岩类麻粒岩
2) high pressure mafic granulite
高压基性麻粒岩
1.
Metamorphic history recorded in high pressure mafic granulites in the Luliangshan Mountains to the north of Qaidam Basin, northwest China: evidence from petrology and zircon SHRIMP geochronology;
柴北缘绿梁山高压基性麻粒岩的变质演化历史:岩石学及锆石SHRIMP年代学证据
3) mafic garnet granulite
石榴基性麻粒岩
1.
On the basis of petrographic evidences, the mineral assemblages in mafic garnet granulite can be divided into three generations: The first stage mineral assemblage is characterized by Opx+Cpx±Hb+Pl±Qz as inclusions in garnet porphy.
蔓箐沟地区石榴基性麻粒岩发育多期变质反应结构。
4) mafic granulite xenoliths
基性麻粒岩包体
5) garnet-bearing granulite
石榴石基性麻粒岩
6) granulite complex
麻粒岩杂岩
1.
The Yishui granulite complex of middle to late Archaean (with isotopic ages ranging be-tween 3000 Ma and 2500 Ma)consists of the supracrustal rocks of Yishui Group and its in-truded charnockites-granitoids.
山东沂水麻粒岩杂岩中含有大量高密度富ＣＯ＿２流体包裹体，伴随有ＣＯ＿２－Ｈ２Ｏ，ＣＯ＿２±Ｎ＿２±ｃＨ＿４的包裹体。
补充资料：麻粒岩
| 麻粒岩 granulite 一种变质岩。又称粒变岩。属中高级区域变质作用产物。1803年魏斯首次命名。主要由长石、石英、辉石 (紫苏辉石、透辉石等）组成，有时含石榴石、矽线石、蓝晶石等。岩石中含水矿物不稳定，一般不含或少含。矿物多呈粒状，组成粗细条带，相间排列，形成麻粒结构。可根据暗色矿物含量分为两种类型：①暗色麻粒岩。暗色矿物 (紫苏辉石、透辉石、角闪石)达30％～80％。② 浅色麻粒岩，暗色矿物含量小于30％。通常认为，其变质作用属于典型的麻粒岩相的范围。有人主张只把具麻粒岩相典型矿物组合的变质岩称作麻粒岩。主要分布在太古宙至早元古代变质岩系中。
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参考词条