吉林地质
吉林地質
길임지질
JILIN GEOLOGY
2013年
4期
51-53
,共3页
周志宇%李翱鹏%张晓锦
週誌宇%李翱鵬%張曉錦
주지우%리고붕%장효금
九三沟%金矿床%地质特征
九三溝%金礦床%地質特徵
구삼구%금광상%지질특정
Jiusangou%gold deposit%geological features
吉林汪清九三沟金矿受东西向断裂控制,以角砾岩筒为中心形成较明显的蚀变分带。金矿体均赋存于角砾岩筒内。该角砾岩筒具隐爆成因特征。本文通过对九三沟金矿地质特征的阐述,为区域找矿提供了参考典型。
吉林汪清九三溝金礦受東西嚮斷裂控製,以角礫巖筒為中心形成較明顯的蝕變分帶。金礦體均賦存于角礫巖筒內。該角礫巖筒具隱爆成因特徵。本文通過對九三溝金礦地質特徵的闡述,為區域找礦提供瞭參攷典型。
길림왕청구삼구금광수동서향단렬공제,이각력암통위중심형성교명현적식변분대。금광체균부존우각력암통내。해각력암통구은폭성인특정。본문통과대구삼구금광지질특정적천술,위구역조광제공료삼고전형。
Jiusangou gold deposit is controlled by EW faults, the obvious alteration zoning center on breccia pipe. Gold ore bodies are hosted in breccia pipe. The breccia pipe has cryptoexplosion origin feature. This paper elaborated geological features of Jiusangou gold deposit that provides a reference for the regional prospecting.