摘要
政和马仑头地区是福建省重要的金银多金属成矿远景区之一,位于东坑火山盆地西北边缘,具有良好的找矿前景。通过对矿区地质特征、矿体特征、矿石特征的分析,推断矿床成因为受北西向断裂和裂隙控制富集成矿,属中低温热液交代-充填型金矿床。
The Maluntou area, located at the northwest edge of Dongkeng volcanic basin, is one of important gold and silver polymetal metallogenic prospective areas and is provided with a favorable ore prospecting. Based on the characteristics of geology, orebody and ore materials in the mining area, it is inferred that the ore deposit is controlled and enriched by the northwest-trend faults and fissures and that it belongs to the gold deposit of intermediate and low temperature hydrothermal replacement-filling type.
出处
《福建地质》
2006年第4期180-184,共5页
Geology of Fujian
关键词
马仑头金矿
地质特征
成因探讨
福建政和
Matoulun Gold Deposit, geologic characteristics, genesis, Zhenghe County
