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地球学报  2009 

豫西小秦岭—熊耳山地区金矿成矿物质来源研究——兼论中基性岩墙与金成矿作用关系

DOI: 10.3975/cagsb.2009.01.05

Keywords: 金矿床,成矿物质来源,岩墙,壳幔相互作用,小秦岭—熊耳山地区,秦岭造山带

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Abstract:

小秦岭—熊耳山金矿区是我国重要岩金产地之一。对豫西小秦岭—熊耳山地区金矿床成矿物质来源的可能矿源层分析、同位素和稀土元素示踪等多方面的研究表明，太古代太华群结晶基底、燕山期花岗岩类、中生代中基性岩墙都不是金的成矿物质源区。该地区成矿物质来自于造山带环境下壳幔相互作用过程中的多种相关地质体，成矿流体主要来自于地幔。中基性岩墙没有为金矿床提供成矿物质或热液流体，金成矿作用与岩墙的关系主要表现在二者都形成于发生强烈壳幔相互作用的区域构造环境下，从这种意义上来说，二者是“共栖”关系。

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