南京大学学报(自然科学版) ›› 2018, Vol. 54 ›› Issue (2): 221–.
• • 下一篇
宋谢炎*，胡瑞忠，陈列锰
Song Xieyan*，Hu Ruizhong，Chen Liemeng
摘要： 我国岩浆硫化物矿床类型比较齐全，产出的构造背景比较复杂，尽管铂族元素矿床比较匮乏，但铜镍矿床资源总量名列世界前茅. 不仅在华北克拉通西南缘和峨眉大火成岩省发现了一系列与地幔柱岩浆活动有关的铜镍(铂族元素)矿床，例如金川和杨柳坪超大型铜镍铂族元素矿床；还在中亚造山带南缘境内以及东昆仑造山带发现了一批规模可观的铜镍矿床，甚至超大型矿床，例如夏日哈木超大型镍钴矿床，使得我国产于板块聚合边界铜镍矿床在镍资源总量中所占的比例远高于世界平均值. 这种特点一方面取决于我国特殊的地质背景，反映了我国铜镍矿床成因的特点；另一方面也说明我国这类矿床的勘查策略和技术具有优势，我国地质工作者卓有成效的找矿实践极大地丰富了铜镍硫化物矿床的找矿理论，拓展了这类矿床的找矿空间. 对华北克拉通、峨眉大火成岩省、中亚造山带南缘及东昆仑造山带已发现矿床的地质特征进行总结，对于未来这些区域找矿潜力的合理评价及预测是非常重要的．
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