安徽地质
安徽地質
안휘지질
GEOLOGY OF ANHUI
2013年
4期
256-260
,共5页
枞庐盆地%陶家巷%工区%物化探%矿化蚀变%成矿
樅廬盆地%陶傢巷%工區%物化探%礦化蝕變%成礦
종려분지%도가항%공구%물화탐%광화식변%성광
Zong-Lu basin%Taojiaxiang%mining site%geophysical and geochemical survey%mineralized alteration%mineral-ization
本文对枞阳县陶家巷工区成矿地质特征,物化探特征,地球化学特征,矿化蚀变特征等进行分析,研究显示区内成矿元素 Cu、Pb、Zn 等含量高于地壳背景值,断裂构造发育,断裂带内铜矿化、硅化等明显。断层发育,NE向断层发育,多以硅化带形式出现。裂隙发育,具不同程度的硅化高岭土化,局部充填有褐铁矿化脉。陶家巷-高庙山低缓异常带、方家湾地存在重磁同高异常,与已知矿化含铜破碎带重合。结果表明,陶家巷大刨山铜矿深部及外围、城山岩体与围岩接触带、夏家井、方家湾、五印庵-团山小学和高庙山具有较好的找矿潜力。
本文對樅暘縣陶傢巷工區成礦地質特徵,物化探特徵,地毬化學特徵,礦化蝕變特徵等進行分析,研究顯示區內成礦元素 Cu、Pb、Zn 等含量高于地殼揹景值,斷裂構造髮育,斷裂帶內銅礦化、硅化等明顯。斷層髮育,NE嚮斷層髮育,多以硅化帶形式齣現。裂隙髮育,具不同程度的硅化高嶺土化,跼部充填有褐鐵礦化脈。陶傢巷-高廟山低緩異常帶、方傢灣地存在重磁同高異常,與已知礦化含銅破碎帶重閤。結果錶明,陶傢巷大鑤山銅礦深部及外圍、城山巖體與圍巖接觸帶、夏傢井、方傢灣、五印菴-糰山小學和高廟山具有較好的找礦潛力。
본문대종양현도가항공구성광지질특정,물화탐특정,지구화학특정,광화식변특정등진행분석,연구현시구내성광원소 Cu、Pb、Zn 등함량고우지각배경치,단렬구조발육,단렬대내동광화、규화등명현。단층발육,NE향단층발육,다이규화대형식출현。렬극발육,구불동정도적규화고령토화,국부충전유갈철광화맥。도가항-고묘산저완이상대、방가만지존재중자동고이상,여이지광화함동파쇄대중합。결과표명,도가항대포산동광심부급외위、성산암체여위암접촉대、하가정、방가만、오인암-단산소학화고묘산구유교호적조광잠력。
In view of geological, geophysical, geochemical and mineralized alteration features of the Taojiaxiang mining site in Zongyang County, this paper found that Cu, Pb and Zn contents are remarkably higher than the background val-ues, fracturing structures are developed and host marked copper mineralization and silication. The NE faults are devel-oped, mostly in the form of silication zone. Rifts are developed with varying degrees of silication and kaolinization, lo-cally filled with ferritized veins. The Taojiaxiang-Gaomiaoshan low gentle anomalous belt and both high gravitational and magnetic anomalies in Fangjiawan overlap with the known mineralized copper-bearing fracture zone. The results in-dicate good potential for ore prospecting in depth of the Dabaoshan copper mine and the periphery in Taojiaxiang, the contact between the Chengshan intrusion and wall rock, Xiajiajing, Fangjiawan, Wuyinan-Tuanshan Primary School and Gaomiaoshan.