摘要
甘肃省肃北县公婆泉东铁铜矿区属于公婆泉岩浆弧,位于勒巴泉-公婆泉成矿带,该成矿带地质构造和岩浆作用十分发育,经历了多期次、多阶段的成矿作用,矿产资源十分丰富。特别在公婆泉东一带磁异常较强,铜元素地球化学异常明显,本文通过分析公婆泉东及附近的地质背景,研究其铁铜矿的成矿潜力,为后续找矿提供参考。
Gongpoquan east iron-copper mine area in Subei County,Gansu province belongs to Gongpoquan magmatic arc and is located in Lebaquan Gongpoquan metallogenic belt.The geological structure and magmatism of the metallogenic belt are well developed,which has experienced multi-epoches and multi-stage mineralization,and the mineral resources are very rich.Especially in the east zone of Gongpoquan,the magnetic anomaly is strong,and the geochemical anomaly of copper element is obvious.This paper analyzed the geological background of Gongpoquan East and its vicinity,studied the metallogenic potential of iron-copper deposits,and provided a reference for subsequent ore exploration.
作者
徐磊
XU Lei(Geological Survey Institute of Gansu Province,Lanzhou 730000,Gansu,China)
出处
《资源信息与工程》
2020年第3期4-6,共3页
Resource Information and Engineering
关键词
公婆泉
铁铜矿
成矿潜力
Liangjiazi
iron-copper deposit
metallogenic potential
