首页> 外文会议>12th international nickel symposium >Genesis of Zoned Amphibole and its Relationship with the PGE Mineralization in the Wengeqi Mafic-ultramafic Complex,Guyang Country,Inner-Mongolia,China
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Genesis of Zoned Amphibole and its Relationship with the PGE Mineralization in the Wengeqi Mafic-ultramafic Complex,Guyang Country,Inner-Mongolia,China

机译:内蒙古自治区阳阳市温格奇镁铁质-超镁铁质复合带中闪石的成因及其与PGE矿化的关系

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摘要

1 INTRODUCTIONThe Wengeqi mafic-ultramafic complex is located in Guyang County,Inner Mongolia,in the central part of northern margin of the North China craton (Fig.1a).The intrusion extends 3.5 km NW-SE and 1.5 km NE-SW (Fig.1b).The area of the Complex is approximately 5.0 km2 (Figure 1).
机译:1引言温格奇镁铁质-超镁铁质复合体位于内蒙古古阳县,在华北克拉通北缘的中部(图1a),侵入带延伸了北西向东南3.5公里和南北向1.5公里(图1a)。 .1b)。综合大楼的面积约为5.0平方公里(图1)。

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  • 来源
  • 会议地点 Guiyang(CN)
  • 作者单位

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

    China University of Geosciences,Beijing,100083;

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