摘要
太山庙金矿位于栗扎坪—七里峡区域性大断裂(F1)的南盘,该断裂旁侧次级平行的构造提供了很好的成矿空间,矿区的岩浆侵入为成矿提供良好的成矿热液,近矿围岩为下志留统大贵坪组第二段,含矿岩石为石英脉,成因类型为岩浆热液型矿床,工业类型为石英脉型金矿。
Taishanmiao Au deposit is in the S wall of Lizaping-Qilixia regional megafault(F 1).The secondary parallel structure provides the good space for the metallogenesis.The magma intrusion in the orefield provides the good hot fluid for the metallogenesis.The wall rock near the orebody is Lower Silurian Daguiping Formation Member 2.The quartz vein is the ore-bearing body.It is the magma hydrothermal deposit in genesis,and the quartz vein Au deposit in the industrial type.
作者
刘吉权
文亚松
LIU Ji-quan;WEN Ya-song(Yunnan Weilida Company(Ltd)of Geophysical Exploration,Kunming 650217)
出处
《云南地质》
2018年第1期67-71,共5页
Yunnan Geology
关键词
构造控矿
热液型矿床
陕西宁陕太山庙
Ore Control of Structure
Hydrothermal Deposit
Taishanmiao,Ningshan,Shanxi
