摘要
桃花—石门金矿带位于秦岭地槽区北秦岭纬向褶皱带的北端黑沟和瓦穴子断裂所夹持的前加里东褶皱带中。矿床类型为石英脉型 ,石英脉规模小 ,数量多 ,分布于瓦穴子断裂北侧。矿脉的产出受地层、构造控制 ,成矿与岩性、构造、岩浆活动。
Taohua shimen gold ore belt is located in the Pre caledonian fold belt between Heigou and Waxuezi faults in the North Qinling latitudinal fold belt of the Qinling geosyncline. It is a quartz vein type Au deposit with many small quartz veins in the north side of Waxuezi fault. Ore veins are controled by stratigraphic units and structures. Ore formation is closely related to lithology, structure, temperalure etc.
出处
《地质找矿论丛》
CAS
CSCD
2002年第3期180-185,共6页
Contributions to Geology and Mineral Resources Research
