1) garnet diopsidite
石榴透辉石岩
1.
Most researchers consider that Chijiadian garnet lherzolite in Datan of Shandong Provinceincludes mainly eclogite composed chiefly of omphacite + garnet, with small amounts of intercalated garnet diopsidite.
山东大疃迟家店石榴二辉橄榄岩中榴辉岩与石榴透辉石岩呈过渡关系，前者位于中心，后者为边缘带。
2) griquaite
透辉石榴岩
3) sommaite
白榴石;白榴透长辉长岩
4) 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 。
5) garnet clinopyroxenite
石榴单辉辉石岩
1.
Geochemical characteristics of garnet clinopyroxenite at Hujialing,Rizhao,and their bearing on petrogenesis;
日照胡家岭石榴单辉辉石岩体的地球化学特征及其成因
6) pyroxene-garnetite
辉石石榴石岩
1.
However, our results presented in this paper suggest that the pyroxene-garnetite occurring near Hongmiao, North Dabie terrain, underwent amphibole-f acies retrogression after the Triassic UHP metamorphism, n.
本文对北大别安徽洪庙百丈岩榴辉岩相岩石(辉石石榴石岩)的研究表明,该岩石经历了三叠纪超高压变质作用,经历了角闪岩相退变质。
补充资料：透辉石
分子式：CaMg(Si2O6)
CAS号：
性质：CaO约25.9％，MgO约18.5％，SiO2约55.6％，有时含铁、锰、铬等的氧化物。单斜晶系。呈短柱状，其横断面呈假正方形或八边形，集合体呈粒状、柱状、放射状。浅绿或淡灰色，玻璃光泽。中等解理平行{110}，解离面交角为87°或93°。硬度5.5～6，密度3.27～3.38g/cm3。熔点1391℃。广泛分布于基性，超基性岩中，主要矿物为硅卡岩。当玻璃相组成中含氧化镁过高时有透辉石析出。在铬渣铸石及白色铸石中常作为主要组分成矿物出现。用作耐火材料。
CAS号：
性质：CaO约25.9％，MgO约18.5％，SiO2约55.6％，有时含铁、锰、铬等的氧化物。单斜晶系。呈短柱状，其横断面呈假正方形或八边形，集合体呈粒状、柱状、放射状。浅绿或淡灰色，玻璃光泽。中等解理平行{110}，解离面交角为87°或93°。硬度5.5～6，密度3.27～3.38g/cm3。熔点1391℃。广泛分布于基性，超基性岩中，主要矿物为硅卡岩。当玻璃相组成中含氧化镁过高时有透辉石析出。在铬渣铸石及白色铸石中常作为主要组分成矿物出现。用作耐火材料。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条