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- The former three stages reflect the major process of eclogite facies metamorphism and the latest stages the light overprinting of greenschist facies retrometamorphism at the shallow level of crust. 前三个阶段反映了榴辉岩相变质作用的主要过程。后一阶段，反映了榴辉岩在地壳浅部层次绿片岩相环境下遭受轻微的叠加改造。
- Metamorphism, deformation and fluid evolution of the high-pressure eclogite facies metamorphic belts in the northern Hubie province, China 鄂北高压榴辉岩相变质带的变质、变形和流体演化
- eclogite facies 榴辉岩相
- You may call my facies whimsical. 你可以把我这些想法称为异想天开。
- Its facies, structure and geneses are complicated. 其岩相、结构构造、成因复杂。
- They belong to the amphibolite facies. 属于角闪岩相产物。
- The sedimentary members are largely turbidites of greywacke facies. 沉积岩的组成大部分为杂砂岩相的浊积岩。
- Clastic facies pattern recognition is somewhat systematic. 碎屑岩相模式的识别是带有一定系统性的。
- The sediments are detrital and largely of greywacke facies. 沉积岩为碎屑质，大部分属于杂质砂岩相。
- The orebearing sequence is littoral-lagoon sedimentary facies. 层状、似层状铝土矿规模大、品位高,主要分布于豫西地区;
- Green is a low-level multi-amphibolite facies of the green. 绿岩多属低级角闪岩相到绿片岩相。
- Clastic facies pattern recognition is somewhat systematic . 碎屑岩相模式的识别是带有一定系统性的。
- The upper subfacies of effusive facies is the best reservoir. 其中喷溢相上部亚相是储层物性最好的岩相带。
- Metamorphic facies map of Taiwan. Spec. Publ. Geol. Surv., 2, 32p. 陈肇夏、朱效祖(1983)台湾变质相图。经济部中央地质调查所特刊，第2号，附图。
- Oceanic subduction-type eclogite in the Lhasa block, Tibet, China:Remains of the Paleo-Tethys ocean basin? 青藏高原拉萨地块中的大洋俯冲型榴辉岩:古特提斯洋盆的残留?
- Facies of species are often connected with extreme or disturbed habitats. 植物种的群常与严酷或干扰的生境有联系。
- Microstructures of the garnet vary greatly from coesite-bearing eclogite to quartz eclogite and garnet amphibolite. 在含柯石英榴辉岩中的石榴子石位错密度比角闪岩中的低。
- Strong tectonism is thought to have made a great contribution to the formation of eclogite in the Dabie UHPM zome. 同位素资料分析表明，大别地区榴辉岩系地壳成因，这对于榴辉岩是壳内产物的认识提供了进一步证据。
- Abundant eclogite xenoliths are found in Mesozoic dioritic rocks from Xuzhou-Suzhou area, central China. 摘要徐州-宿州地区中生代闪长质岩石中存在丰富的榴辉岩类捕虏体。
- Dr. Xu Zhiqin, a Chinese geologist, first discovered coesite in the eclogite in the west of Tianzhu mountain in 1987. 1987年，我国地质学家许志琴首先在天柱山西边榴辉岩中发现柯石英。
