甘肃天鹿砂岩型铜矿床地质特征及成矿模式
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引用本文:.2006.Geological characteristics and metallogenetic model of Tianlu sandstone copper deposit in Gansu Province [J].Mineral Deposits,25(3):312~320
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李大民,孙永君,许文进 甘肃省地质矿产勘查开发局第四地质矿产勘查院 
基金项目:甘肃省地质矿产局切块基金项目(K1.10)
中文摘要:文章在系统总结天鹿铜矿床地质特征的基础上,分析了成矿时代和矿床成因,并建立了成矿模式。结果表明,天鹿铜矿床赋存于中志留统泉脑沟山组杂色岩层中,其成矿物质来自陆源,主成矿期为中志留世,属沉积砂岩型铜矿床。
中文关键词:地质学  砂岩型铜矿床  地质特征  矿床成因  成矿模式  天鹿铜矿床
 
Geological characteristics and metallogenetic model of Tianlu sandstone copper deposit in Gansu Province
Abstract:Based on systematic summarization of geological characteristics of the Tianlu copper deposit, this paper has analyzed its metallogenic epoch and genesis, and built up a metallogenic model. The results show that the ore_bearing strata occur in variegated strata of Middle Silurian Quannaogoushan Formation, that the metallogenic materials might have been derived from the land area, and the metallogenic epoch is middle Silurian.
keywords:geology, sandstone copper deposit, geological characteristics, genesis of ore deposit, metallogenic model, Tianlu copper deposit
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