吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (1): 53-69.doi: 10.13278/j.cnki.jjuese.20160299
唐文龙, 孙宏伟, 刘晓阳, 王杰, 左立波, 吴兴源
Tang Wenlong, Sun Hongwei, Liu Xiaoyang, Wang Jie, Zuo Libo, Wu Xingyuan
摘要： 中南部非洲镍矿资源丰富，大体可分为岩浆型和风化壳型2种预测类型。本文在对中南部非洲243处镍矿床/点资料系统收集整理的基础上，将产出的镍矿初步划分为新太古代、古元古代、中元古代和新元古代4个成矿期，南非卡普瓦尔北缘古元古代Cr-Ni-Cu（PGE）成矿带、津巴布韦大岩墙新太古代Ni-Cr（PGE）成矿带、博茨瓦纳弗朗西斯敦—赛莱比—皮奎新太古代Ni-Cu-Au成矿带、赞比亚赞比西津巴—卢萨卡新元古代Au-Ni-Cu成矿带、坦桑尼亚乌本迪—乌萨嘎仁古元古代Ni-Cu成矿带和坦桑尼亚—布隆迪基巴拉中元古代Ni-Cu-Co成矿带共6个成矿带，从整体上构成了北东向的中南部非洲巨型镍矿带；并分别对研究区内典型的与大陆边缘裂解有关的Ni-Cu（PGE）矿床、与造山带伸展背景有关的Ni-Cu矿床、与地幔柱有关的Ni-Cu（PGE）矿床和风化壳型镍矿床的矿床地质特征和成矿模式进行了研究。综合研究表明，布什维尔德矿集区、津巴布韦大岩墙矿集区、博茨瓦纳弗朗西斯敦—赛莱比—皮奎矿集区、坦桑尼亚—布隆迪穆松加迪—卡邦加矿集区镍矿资源潜力巨大，找矿前景优越。
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