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1)  Garnet-pyroxene granulites
石榴辉石麻粒岩
1.
Garnet-pyroxene granulites occurring in the Northern Dabie mountain are basic granulites.
大别山北部石榴辉石麻粒岩是一种基性麻粒岩,岩石中富含有大量CO_2、CH_4、H_2S、H_2O流体包裹体,及含子晶多相包裹体。
2)  pyrigarnite
石榴二辉麻粒岩
1.
Discovery of pyrigarnite in Western Kunlun;
西昆仑首次发现石榴二辉麻粒岩
3)  garnet mafic granulite
石榴角闪二辉麻粒岩
1.
High-pressure mineral assemblages were identified in zircons separating from garnet mafic granulites in northwevStern Hebei province by the Laser Raman spectroscopy, cathodoluminescence and electron microprobe method.
采用激光拉曼、阴极发光和电子探针技术,确认冀西北石榴角闪二辉麻粒岩锆石中保存早期高压变质包体矿物组合:石榴石(Grt)+单斜辉石(Cpx)+斜长石(Pl)+石英(Qtz)+金红石(Rt)、单斜辉石(Cpx)+斜长石(Pl)+石英(Qtz)和石榴石(Grt)+单斜辉石(Cpx)+斜长石(Pl)+石英(Qtz)。
4)  garnet granulite
石榴石麻粒岩
1.
The Shandong-Jiangsu eclogites suite is characterized by the widespread distribution of different type eclogites, close assocition garnet peridotiet and garnet granulite, widespread development tenacity shearing zone and extendisve emgrge type-A granite of late Yanshan movement and deep vein rock.
鲁苏榴辉岩套以广泛分布各类榴辉岩、密切伴生石榴石橄榄岩、石榴石麻粒岩等高压岩石组合 ,普遍发育韧性变形带 ,大量出露燕山晚期碱性花岗岩及深源脉岩为特征。
5)  garnet pyroxenite
石榴辉石岩
1.
We report an unusual garnet pyroxenite, as a nodule enclosed within kyanite eclogites from Rongcheng, northeastern Sulu UHP metamorphic belt.
在苏鲁超高压变质带荣成蓝晶石榴辉岩中,发现一具有特殊结构和地球化学特征的石榴辉石岩。
2.
The garnet pyroxenites are grass green massive rocks occurred as small pods decimeters in size,embedded in highly serpentinized peridotites.
大别山北坡霍山饶拔寨等地的超基性岩中含有石榴辉石岩的包体。
3.
The detailed investigation into the amphibole two_pyroxene granulite in the north of Dabie metamorphic terrain in terms of petrography, mineral chemistry, petrochemistry, and estimated p_t conditions for metamorphism indicates that this rock is a product of the garnet pyroxenite that experienced the granulite_facies retrograde metamorphism during its uplift.
详细的岩相学、矿物化学、岩石化学和变质作用温压条件计算表明 ,大别变质地体北部角闪二辉麻粒岩是石榴辉石岩在其抬升过程中经历麻粒岩相退变质作用的产物 ,峰期变质作用至少是发生在高压榴辉岩相条件下 ,而且地温梯度较低 。
6)  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。
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。
    
   

麻粒岩

麻粒岩

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