摘要
通过对本区构造断裂带、蚀变带、矿化体、矿体的分析研究,本区的矿体、矿化体严格受控于控矿蚀变带,控矿蚀变带严格受控于控矿构造,属于构造控矿。据矿体、矿化体、控矿蚀变带、控矿构造的产出状态,本区矿体、矿化体均呈近南北向展布,故米山断裂带所派生的次级构造系本区的赋矿构造,指明了找矿方向。
Through the analysis and study of the structural fault zone,alteration zone,mineralized body and orebody in this area,the orebody and mineralized body are strictly controlled by the ore-controlling alteration zone,and the ore-controlling alteration zone is strictly controlled by the ore-controlling structure,which belongs to structural ore-controlling.According to the occurrence state of ore bodies,mineralized bodies,ore-controlling alteration belts and ore-controlling structures,the orebodies and mineralized bodies in this area are all distributed in nearly north-south direction,so the secondary structures derived from the Mishan fault zone are the ore-bearing structures in this area,indicating the prospecting direction.
作者
卢文东
LU Wen-dong(Shandong No.1 Institute of Geology and mineral exploration,Ji＇nan 250100,China)
出处
《世界有色金属》
2018年第15期93-94,共2页
World Nonferrous Metals
关键词
铜矿
控矿构造
蚀变带
文登北黄
米山断裂
Copper deposits
Ore control structure
Alteration zone
Beihuang in Wendeng
Mishan fault
