摘要
浦城管查铜矿位于峡口—古楼北北东向断裂带上,矿体贮存于早元古代麻源群南山组变质岩和晚侏罗世下渡组火山岩中,受北东向断裂构造控制,矿体呈脉状、透镜状产出,为中低温热液充填交代型矿床。
The Guancha copper deposit in Pucheng County is located in the Xiakou-Gulou NNE- trending faulted belt. The ore bodies lay in the meramorphic rocks of Early Proterozoic Nanshan Formation and in the volcano rock of Late Jurassic Xiadu Formation and are controlled by the NE-trending faulted structures. The orebody acts like a veiny and lenticular occurrence. It belongs to the mineral deposit of the intermediate and low temperature hydrothermal filling and metasomatie type.
出处
《福建地质》
2012年第4期315-324,共10页
Geology of Fujian
关键词
铜矿床
地质特征
找矿前景
浦城管查
copper deposit
geological characteristics
prospecting foreground
Guancha
Pucheng
