首页> 外文期刊>Acta Geologica Sinica >The lanshantou kyanite-bearing eclogite with coesite inclusions in the sulu ultrahigh-pressure metamorphic belt and its PTt path
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The lanshantou kyanite-bearing eclogite with coesite inclusions in the sulu ultrahigh-pressure metamorphic belt and its PTt path

机译:苏鲁超高压变质带兰山头蓝晶石辉长岩辉岩岩脉包裹体

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摘要

Coesite inclusions are found in kyanite from the Lanshantou eclogite in the Sulu ultrahigh-pressure(UHP) metamorphic belt. This discovery extends the stable region of kyanite to over 2.4 GPa. As an important UHP metamorphic belt in China, the Sulu eclogite belt is the product of A-subduction induced by strong compression of the Yellow Sea terrane to the Jiaodong-northereastern Jiangsu terrane during the interaction of the Eurasian plate the Palaeo-Pacific plate in the Indosinian. It stretches about 350 km contains over 1000 eclogite bodies.
机译:苏鲁超高压变质带兰山头榴辉岩的蓝晶石中发现了柯氏岩包裹体。这一发现将蓝晶石的稳定区域扩展到2.4 GPa以上。苏鲁榴辉岩带是中国重要的超高压变质带,是欧亚板块与古太平洋板块相互作用过程中,黄海地带强烈挤压胶东-江苏东北地层引起的A向俯冲的产物。印度支那它绵延约350公里,包含1000多个榴辉岩体。

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