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辽宁岫岩五道沟铁矿床地质特征

李忠满 李大中 刘洪涛

地质找矿论丛2012,Vol.27Issue(4):429-432,4.
地质找矿论丛2012,Vol.27Issue(4):429-432,4.DOI:10.6053/j.issn.1001-1412.2012.04.006

辽宁岫岩五道沟铁矿床地质特征

Geological characteristics of Wudaogou Fe deposit in Xiuyuan county of Liaoning province

李忠满 1李大中 1刘洪涛1

作者信息

  • 1. 辽宁省冶金地质勘查局地质勘查研究院,辽宁鞍山114038
  • 折叠

摘要

Abstract

Wudaogou Fe deposit in Xiuyuan county of Liaoning province occurs in metamorphic rocks of Li'eryu formation of Palaeo-proterozoic Liaohe group and is obviously stratobound. Ore bodies contact sharply with the enclosing rock of biotite-hornblende granulite and without strong alteration. Late structure and dioritic dyke cut the ore bodies without destruction. The Fe deposit can be correlated with Yang-lin style Fe deposit regionally and genetically it is a Palaeo-proterozoic volcanic sedimentary-metamorphic Fe deposit.

关键词

五道沟铁矿/黑云斜长变粒岩/磁铁阳起石岩/辽宁群里尔峪组/辽宁省

Key words

Wudaogou Fe deposit/ biotite-hornblende granulite/ magnetite-actinolite rock/ Li'eryu formation of Palaeo-proterozoic Liaohe group/ Liaoning province

分类

天文与地球科学

引用本文复制引用

李忠满,李大中,刘洪涛..辽宁岫岩五道沟铁矿床地质特征[J].地质找矿论丛,2012,27(4):429-432,4.

地质找矿论丛

OACSCDCSTPCD

1001-1412

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