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The Characteristics and tectonic significance of Permian Volcanic Rocks in Habudala Mountain of alashan right banner, Inner Mongolia

机译:内蒙古阿拉罕右横幅Habudala山山岩石的特点和构造意义

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The Permian volcanic rocks of habudala Mountain in the east-central Inner Mongolia, are a set of radicle-acidity volcanic rocks. The volcanic rocks characteristics of occurrence, petrology, petrochemistry and geochemistry characteristics of metamorphic volcanic rocks are studied in the paper. The research results indicate the volcanic rocks are of the calc-alkaline volcanic rocks characteristics of active continental margins. The model of rare earth element (REE) of the basic volcanic rocks shows that their rock-forming elements came from upper mantle or originated from an old earth crust. Based on the research of rock-forming environment and the regional geological researches, The volcanic rocks in this region belong to a set of the central intraplate eruption of volcanic type, and probably are the outcome of intraplate hot spot or mantle plume.
机译:在内蒙古东部中部的Habudala山的二叠系火山岩是一组胚根酸度火山岩。本文研究了变质火山岩的发生,岩石学,石化和地球化学特征的火山岩特征。研究结果表明,火山岩是钙碱性火山岩岩石的有源大陆边缘的特征。基本火山岩的稀土元素(REE)模型表明,它们的岩石形成元素来自上部地幔或起源于旧地壳。基于岩石形成环境和区域地质研究的研究,该地区的火山岩属于一套火山型中央血管内爆发,可能是血管内热点或披风羽流的结果。

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