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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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Source :
地球学报
ISSN: 1006-3021
CN: 11-3474/P
Year: 2010
Issue: 2
Volume: 31
Page: 209-215
Cited Count:
SCOPUS Cited Count:
ESI Highly Cited Papers on the List: 0 Unfold All
WanFang Cited Count:
Chinese Cited Count:
30 Days PV: 3
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