摘要
金水泉金矿赋矿地层为中泥盆地层,位于两条断裂交汇部位。中、酸性浅成小岩体或岩脉附近,以及碳酸盐化、硅化、褐铁矿化等蚀变,是重要的找矿标志。该矿为与韧性剪切带有关的中低温变质热液型蚀变岩型+石英脉型金矿床。
The Jinshuiquan gold deposit is situated in the intersection of two faults in the Middle Devonian System.The alteration of medium,acidic and shallow rock masses and/or veins,as well as carbonation,silicification and limonitization,is an important ore-prospecting marker.The ore deposit is of medium-low temperature metamorphic hydrothermal alteration rock type and quartz vein type gold deposit,which is associated with ductile shear zones.
引文