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。
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.
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基金项目:甘肃省地质矿产局切块基金项目（K1.10）
引用文本：
李大民，孙永君，许文进.2006.甘肃天鹿砂岩型铜矿床地质特征及成矿模式[J].矿床地质,25(3):312~320.2006.Geological characteristics and metallogenetic model of Tianlu sandstone copper deposit in Gansu Province [J].Mineral Deposits25(3):312~320
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