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首页> 外文会议>12th international nickel symposium >Petrogenesis of the Poyi mafic-ultramafic layered intrusion,NE Tarim Basin
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Petrogenesis of the Poyi mafic-ultramafic layered intrusion,NE Tarim Basin

机译：塔里木盆地波依镁铁质-超镁铁质层状侵入岩的成因

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摘要

The Pobei intrusion is located in northeastern Tarim Basin and includes five-stages magmatism.The third stage mainly form ultramafic rocks-dominated layered intrusion,such as Poyi and Poshi intrusions.The Poyi intrusion is mainly composed of ultramafic rocks.
机译：坡北侵入体位于塔里木盆地东北部，包括五个阶段的岩浆作用，第三阶段主要形成以超镁铁质岩为主的层状侵入体，如波依岩和波氏岩体，波依岩体主要由超镁铁质岩组成。

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  • 来源
  • 会议地点 Guiyang(CN)
  • 作者

    Ming-Zhe Xia; Chang-Yi Jiang; Na-Xin Guo; Yan-Fang Song;

  • 作者单位

    Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education,Chang'an University,Xi'an 710054,China;

    Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education,Chang'an University,Xi'an 710054,China;

    Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education,Chang'an University,Xi'an 710054,China;

    Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education,Chang'an University,Xi'an 710054,China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 P578.24;
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