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榴辉岩转化成含帘石的斜长角闪岩。As a result, the eclogite was transformed to epidote-bearing amphibolite.

该俯冲板片熔融前通常变质为含水的榴辉岩。The subducted slabs was metamorphosed to water-bearing eclogite before being melted.

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超高压榴辉岩在地幔对流、壳-幔物质循环和俯冲带动力学起着重要作用。Eclogite plays an important role in mantle convection and dynamics in subduction zone.

石榴子石以铁铝榴石和钙铝榴石为主，属于C类榴辉岩。The garnets consist mainly of almandine and grossularite, and belong to C-type eclogite.

在与该大理岩共生的榴辉岩中，我们发现了磷灰石的磁黄铁矿出溶结构。The eclogite coexisting with this UHP marble contains apatites showing exsolution texture.

榴辉岩型金红石矿是我国近两年新发现的一种矿床类型。The Donghai eclogite type rutile deposit is a new type of ore deposit recently discovered in China.

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。Abundant eclogite xenoliths are found in Mesozoic dioritic rocks from Xuzhou-Suzhou area, central China.

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榴辉岩原始特征保存完好，仅遭受轻微的退变质作用和叠加变质作用。The eclogite remains well its original characteristics, which has only suffered slight retrogressive metamorphism.

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。Microstructures of the garnet vary greatly from coesite-bearing eclogite to quartz eclogite and garnet amphibolite.

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。Dr. Xu Zhiqin, a Chinese geologist, first discovered coesite in the eclogite in the west of Tianzhu mountain in 1987.

在中国大陆科学钻探主孔榴辉岩中发现了重晶石。Barite was found as inclusions in garnet of eclogite from the main borehole core of the Chinese Continental Scientific Drilling.

二者变质作用P-T参数的差异归因于抬升过程中退变质反应速度的不同。Eclogite has a different velocity of retrograde metamorphic reactions, so a different P-T path from gneisses during uplift process.

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岩体内的石榴辉石岩和榴辉岩包体，具高温成因的特点。The eclogite and garnet pyroxenite enclaves are of high-temperature genesis and are products of partial melting of the upper mantle.

榴辉岩与围岩片麻岩的过渡关系也证实，超高压变质的榴辉岩体是“原地”形成的。The transition relationship between the eclogite and gneiss matrix also clearly shows that the eclogites were metamorphosed in situ.

说明在加里东期北秦岭造山带发生过高压变质事件。Eclogite and coesite-bearing ecloGite occur in the northern part of the Qinling complex inthe Guanpo area, northern Qinling mountains.

榴辉岩的流变性质和变形机制对于阐明大陆造山带和大陆深俯冲的动力学过程具有十分重要的意义。Information on eclogite rheology is of great implication for understanding of collision belts and the deeper levels of subducted zone.

安徽大别、苏北和山东胶南是世界上第三个发现含柯石英榴辉岩的地区。The coesite-bearing eclogite samples were collected from the Bixiling body of Yuexi County, Anhui Province, part of the Dabie Mountains.

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河南大别山区含柯石英榴辉岩的发现扩大了中国中东部含柯石英榴辉岩带的分布区。The discovery of coesite -bearing eclogites in this area enlarges the region of coesite-bearing eclogite belt in Central -Eastern China.

这些认识对解释分布于大别山—东秦岭造山带中的榴辉岩的形成及折返时间与机制提出疑问。All the above views cast doubt on the formation and exhumation mechanism and timing of eclogite in the Dabie -East Qinling orogenic belt.

胶南隆起含榴辉岩高压变质带为大别超高压带的东延部分。The eclogite bearing high pressure metamorphic belt in the Jiaonan uplift is the eastward extension of the Dabie ultra high pressure belt.