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中国祖母绿矿床特征及其找矿方向

THE CHARACTERISTICS AND PROSPECTING DIRECTION OF THE EMERALD DEPOSIT IN CHINA

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【作者】 冯明刚张世涛吕伟

【Author】 Feng Minggang Zhang Shitao Lu Wei (Regional Geological and Mineral Resources Investigation Team, Yunnan Geo-Exploration Bureau, Yuxi 653100)

【机构】 云南省地勘局区域地质调查大队!玉溪653100

【摘要】 中国祖母绿 ,产于南温河变质核杂岩的变质内核中 ,含矿构造有两种 :一为长英质伟晶岩脉 ,一为顺面理产生的石英脉。后者所产祖母绿质量较好 ,是祖母绿的主要含矿构造。经研究 ,构成祖母绿的主要元素Be ,主要来自燕山期花岗斑岩 ,而致色元素Cr和V主要来源于元古界变粒岩。矿区外围仍有很好的找矿远景 ,找矿靶区应选在变质核杂岩内核中的元古界层状变质岩系。

【Abstract】 The China emerald is occurred in the metamorphic core of the Nanwen River metamorphic complex. The ore-bearing structures consist of felsic pegmatite vein and quartz vein along schistosity. And the quality of the emerald occurred in the latter ,is better, which is the main ore-bearing structure of the emerald. According to the study, the main element Be of emerald is derived mostly from Yanshanian granite-prophyry whereas the coloring elements Cr and V are mostly from the Proterozoic granulite. The prospecting potentiality is good as well outside the ore-field. And the prospecting target must be selected in the Proterozoic bedded metamophic rock series of the metamorphic core.

  • 【文献出处】 云南地质 ,YUNNAN GEOLOGY , 编辑部邮箱 ,2000年01期
  • 【分类号】P619.281
  • 【被引频次】27
  • 【下载频次】359
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