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该金矿平均品位48克/吨,最高可达137克/吨,现已探明一定储量。自然金呈树枝状、粒状和不规则状与褐铁矿连生。矿床位于北东向麻城—团风断裂带东侧,大别山金银多金属矿区西北部。含金石英脉主要赋存于大别群铁冶组中段斜长角闪岩夹薄层片麻状混合岩的破碎带内。破碎带近东西向,见有绿泥石化,褐铁矿化和弱硅化。含金石英脉产状与破碎带基本一致,脉体形态简单、
The average gold grade of 48 grams / ton, up to 137 grams / ton, has proven reserves. Natural gold was dendritic, grainy and irregular with limonite even students. The deposit is located to the east of Macheng-Tuanfeng fault zone in the north east and to the northwest of the Dabieshan gold, silver and polymetallic ore district. The gold-bearing quartz veins mainly occur in the crustal zone of the slab-hosted gneissic rocks in the middle part of the Tiede Formation in the Dabie Group. Broken zone near east-west, see chlorite, limonite mineralization and weak silicification. Gold-bearing quartz veins and rupture zone is basically the same pulse body morphology is simple,