吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (5): 1365-1383.doi: 10.13278/j.cnki.jjuese.201505110
陈大
Chen Da
摘要:
为探索川滇黔相邻区铅锌矿床之成因规律,提升成矿理论认识及预测找矿效果,通过对区内铅锌矿床分布规律研究得出如下认识:1)发现矿床(点)之集群分布趋势,据此将成矿区域划分为3个矿集区;2)统计发现,震旦系和石炭系具有较高的成矿机率(51.57%),灯影组和摆佐组汇聚了区域80.98%的金属量;3)构造单元分级控制了成矿单元展布,而矿集区与二级构造单元之间具有不完全的对等性,矿集区Ⅰ、Ⅱ由康滇地轴和龙门山拗陷及二者向上扬子区域跨越地带联合控制;4)根据菱(赤)铁矿与铅锌矿空间耦合,以及菱(赤)铁矿伴生铅锌元素、铅锌矿物含量均较高等现象,论证了在盆地演化早期,古陆边缘拗陷带(或海盆)内之次级单元代表了浅海环境之低能较深水凹(断)陷或海湾环境,沉积了古生界志留系兰多维列统特列奇阶至下石炭统德坞阶和中元古界下昆阳群(会理群)两套含铁建造,形成了区域Pb、Zn成矿金属元素的初始富集,并于成岩-后生期经热液流体循环改造而成矿,含铁建造提供了成矿的主要矿质来源;5)本区成矿物质硫源-膏盐层主要赋存于灯影组和摆佐组下伏地层以及寒武系多个层位;6)矿源层、硫源共同决定了矿集区以及层控的形成机制,并成为控制其分布的决定性因素。
中图分类号:
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