华南地质与矿产
華南地質與礦產
화남지질여광산
GEOLOGY AND MINERAL RESOURCES OF SOUTH CHINA
2015年
1期
61-66
,共6页
金矿床%地质特征%找矿标志%石头坂
金礦床%地質特徵%找礦標誌%石頭坂
금광상%지질특정%조광표지%석두판
geological characteristics%prospecting criteria%Shitouban gold deposit
石头坂金矿位于闽东火山断拗带的西部，是该成矿区带发现的重要金矿床。通过对石头坂金矿床地质特征的分析研究，认为其矿床成因类型属岩浆期后中低温热液矿床，并系统总结了找矿标志。
石頭坂金礦位于閩東火山斷拗帶的西部，是該成礦區帶髮現的重要金礦床。通過對石頭坂金礦床地質特徵的分析研究，認為其礦床成因類型屬巖漿期後中低溫熱液礦床，併繫統總結瞭找礦標誌。
석두판금광위우민동화산단요대적서부，시해성광구대발현적중요금광상。통과대석두판금광상지질특정적분석연구，인위기광상성인류형속암장기후중저온열액광상，병계통총결료조광표지。
The Shitouban gold deposit is located in the western of east Fujian fracture depression and it's an important discovery of prospecting work. By analyzing the geological characteristics of the deposit, it is re-vealed that the gold deposit is a medium low temperature hydrothermal ore deposit after the magma period. The prospecting criteria are concluded as well.
