摘要
满丈岗地区在海西晚期以来,伴随着火山岩的大量喷出、岩浆的侵入、构造运动的频繁发生,为金矿的形成提供了矿质、热动力及导矿、容矿空间。满丈岗金矿的矿源层为上三叠统德亥龙酸性火山岩组。控矿构造主要为NNW向的断裂构造。综合分析区内化探异常、金矿(化)体及矿体类型,找出了区内找金前景。
Along with the volcanic massive eruption, magma intrusion, the frequent occurrence of tectonic movement, Manzhanggang regional provides mineral, thernal power, and ore-guided, ore-containing space for the formation of gold deposit since late Hercynian. The mineral orginal layer of Manzhanggang gold deposit is Upper Triassic acidic volcanic rock. Ore-controlling structure is mainly to the north-northwest faults. This paper analyse the geochemical anomaly, gold ore body and its type of this area comprehensively, and raise the prospecting potential of gold deposit.
出处
《黄金科学技术》
2008年第5期27-28,43,共3页
Gold Science and Technology
关键词
满丈岗
金
找矿前景
成矿条件
Manzhanggang
Gold
Prospecting potential
Metallogenic condition
