摘要
团结沟金矿区花岗斑岩为岩株状产出的浅成超浅成侵入体。斑岩体内有两期矿化;早期发生在隐爆角砾岩带内,呈环形分布;晚期发生在北西西、北北西构造带内。斑岩体不仅提供成矿热液,也提供部分矿质。
The granite porphyry occurred in TuanJieGou Gold Field is rock plant like hypabyssal/super hypabyssal intrusive mass.Two phases of mineralization took place in porphyry mass.The early phase of it took place in the belt of concealed explosive breccia presenting ringlike distribution while the later phase of it happened in the northwest by west/northwest by north structural belt.The porphyry mass provided not only mineralizing hydrothermal solution but also a part of mineral matter.
出处
《黄金》
CAS
北大核心
1998年第3期3-6,共4页
Gold
关键词
斑岩体
隐爆角砾岩
金矿床
叠加矿化
金矿
porphyry mass
concealed explosive breccia
northwest by west/northwest by north structural belt
superimposed mineralization
TuanJieGou Gold Deposit