摘要
大金山铅锌矿位于泰宁—政和北东东向铜多金属成矿带上,是该成矿带主要的矿种之一,也是闽北地区一个较有价值的矿床。矿床产于早元古代南山组上段,受燕山期北东东向构造控制,属中低温热液充填交代型矿床。
The Dajinshan Lead-zinc Deposit, situated at the copper polymetal metallogenetic belt of Taining-Zhenghe north-east-east trend, is one of valuable mineral deposits in Northern Fujian. It exists in the upper segment of Early Proterozoic Nanshan Formation strata and is controlled by the north-east-east structures of Yanshanian Stage. The deposit belongs to the ones of the intermediate and low temperature hydrothermal filling and metasomatic type.
出处
《福建地质》
2008年第4期377-384,共8页
Geology of Fujian
关键词
铅锌矿床
地球物理
地球化学
异常
建阳大金山
lead-zinc deposit, geophysics, geochemistry, anomaly, Jianyan County
