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东秦岭熊耳山地区骆驼山硫多金属矿床赋存规律及成因研究

Analysis on Causes and Occurrence Regularity of Luotuoshan Sulfide Polymetallic Deposit

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【作者】 权知心李香资付恒一张蓓袁征付治国

【Author】 QUAN Zhi-xin;LI Xiang-zi;FU Heng-yi;ZHANG Bei;YUAN Zheng;FU Zhi-guo;No.2 Geo-exploration Institute Henan Provincial Bureau of Geo-exploration and Mineral Development;

【机构】 河南省地质矿产勘查开发局第二地质勘查院

【摘要】 总结归纳骆驼山硫多金属矿床的赋存规律和成因,主要是通过介绍矿床的控矿地质条件、赋存规律、矿床成因、成矿作用,以期为采用类比法寻找同类型的硫多金属矿床提供经验;矿床产于新元古界青白口系栾川群三川组大理岩所夹矽卡岩带中。矿体呈大的透镜状,产状与矽卡岩带展布规律一致;矿床矿种多,组份复杂,共生矿产主要有S、Cu、Wo3、Zn、Ca F2,伴生有益组分有Be、Cd、In、Ag等,以密集块状和浸染状矿石为主,矿床工业综合利用价值相对较高。

【Abstract】 Summarize the occurrence regularity and causes of Luotuoshan sulfide polymetallic deposit,including introduce the ore-controlling geological conditions,regularity of occurrence,origin and mineralization,so as to seek the same type of sulfide polymetallic deposit by analogy; it was originated from Neoproterozoic erathem,in the marble skarn zone of Luanchuan-Sanchuan group,Qingbaikou system. The ore body was shaped in large lenticular,and the occurrence was no difference from skarn zone distribution; with many types of deposits and complex components,paragenetic minerals mainly are S,Cu,Wo3,Zn,Ca F2,associated with useful components such as Be,Cd,In,Ag,etc,which mainly were dense massive and disseminated ores,with a high industrial value.

  • 【分类号】P618.2
  • 【下载频次】77
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