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地球学报  2010 

紫金山金铜矿床深部成矿作用研究和找矿前景评价的关键

DOI: 10.3975/cagsb.2010.02.10

Keywords: 热液蚀变帽,高级泥化蚀变带,铜硫化物,蓝辉铜矿,紫金山铜金矿床

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Abstract:

紫金山铜金矿床是典型的高硫化浅成低温热液矿床,发育巨厚的热液蚀变帽,多孔状石英和高级泥化蚀变带等标志性特征;特别是在金矿体之下出现垂直厚度超过1000米的巨大铜矿体,属于蓝辉铜矿-铜蓝-硫砷铜矿-明矾石矿物组合的高硫化型浅成低温热液铜矿床类型,铜硫化物的矿物学研究预示着深部可能变为斑岩型铜矿床。

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