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pillow basalt

  • 枕状玄武岩

网络释义专业释义

短语

altered pillow-basalt 蚀变枕状玄武岩

pillow form basalt 枕状玄武岩

  • 枕状玄武岩 - 引用次数:7

    The ultramafic rocks,cumulate rocks,sheeted dike complex ,pillow basalt are relativelyenriched in LREE,which are distinguished from normal oceanic ophiolite. The sheeted dike 54吉林大学硕士学位论文complex belongs to calc-alkaline series rocks which is consistent with island arc rocks.

    本区蛇绿岩中超镁铁岩、堆晶杂岩、席岩墙群、枕状玄武岩均具有轻稀土富集的特征,区别于标准的大洋蛇绿岩。

    参考来源 - 西藏永珠—纳木错蛇绿岩地球化学特征及其构造环境

·2,447,543篇论文数据,部分数据来源于NoteExpress

双语例句

  • Typical metamorphic pillow basalt is widely distributed in the Liuhang "Formation" of the Taishan "Group", west of Tuanyuangou village, Zhangqiu, western Shandong Province.

    鲁西泰山岩群柳杭岩中,典型变质玄武岩出露济南章丘团员西一带。

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  • The oceanic island basalt is represented by the Nonghuai pillow lava, which is, originally Hawaii type one in the Paleotethyan ocean, an allochthon in the Indosinian foreland fold and thrust belt.

    玄武岩弄槐熔岩为代表性火山岩,原为古特提斯洋盆中的夏威夷洋岛,现保存支期前褶皱冲断带的一个外来岩席中。

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  • The study on petrology, lithochemistry and geo-chemistry of the pillow lava shows that it is the product of submarine basalt.

    熔岩岩石学、岩石化学地球化学研究表明海底玄武岩产物

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