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eclogite facies

  • 榴辉岩相

网络释义专业释义

  [岩] 榴辉岩相

榴辉岩相eclogite facies)是一种高压至超高压区域 变质相。特征岩石为榴辉岩,常呈透镜体产出。

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短语

eclogite-facies 榴辉岩相

eclogite facies rocks 榴辉岩相岩石

eclogite facies metamorphism 榴辉岩相变质作用

eclogite-facies metamorphism 榴辉岩相变质作用

ultrahigh-pressure eclogite-facies rocks 超高压榴辉岩相岩石

Eclogite facies garnet pyroxenolite xenoliths 榴辉岩相石榴辉石岩捕虏体

the granulite-eclogite facies cumulate xenoliths 麻粒岩相

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  • 榴辉岩相 - 引用次数:6

    参考来源 - 冈底斯铜矿带埃达克质含矿斑岩的源区组成与地壳混染:Nd、Sr、Pb、O同位素约束

·2,447,543篇论文数据,部分数据来源于NoteExpress

双语例句

  • The amphiboles of retrogressive metamorphic stages in the granulite and eclogite were mainly formed under the condition of amphibolite facies of medium pressure facies series.

    麻粒榴辉岩退变质阶段主要形成于中压岩相的温条件

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  • The characteristics of three metamorphic stages are as follows: before the eclogite-facies stage which is middle-pressure epidote amphibolite facies;

    三个变质作用阶段特征辉相阶段为中压系绿帘角闪岩相;

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