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平度市大庄子矿区金矿床成因类型探讨
引用本文:郭百创,赵冬冬.平度市大庄子矿区金矿床成因类型探讨[J].地质与勘探,2002,38(4):36-40.
作者姓名:郭百创  赵冬冬
作者单位:中国冶金地质勘查工程总局山东局三队,烟台,264002
摘    要:平度市大庄子矿区存在两种金矿成因类型,即同沉积断裂-层间滑脱蚀变岩型和石英脉型。矿体明显受层间滑脱和断裂控制,硅化,黄铁矿化,方铅矿化明显,强烈。成矿规律突出,成矿预测效果显。

关 键 词:平度市  金矿床  成因类型  成矿模式  层间滑脱  成矿规律  断裂构造
文章编号:0495-5331(2002)04-0036-05
修稿时间:2002年6月28日

DISCUSSION ON THE GENETIC TYPE OF GOLD DEPOSITS IN DAZHUANGZI MINING AREA IN PINGDU CITY
GUO Bai-chuang,ZHAO Dong-dong.DISCUSSION ON THE GENETIC TYPE OF GOLD DEPOSITS IN DAZHUANGZI MINING AREA IN PINGDU CITY[J].Geology and Prospecting,2002,38(4):36-40.
Authors:GUO Bai-chuang  ZHAO Dong-dong
Abstract:There are two genetic types of gold deposits in Dazhuangzi mining area in Pingdu city, which are the synsedimentary fault-interlayer gliding altered rock type and quartz vein type. The gold orebody are obviously controlled by the interlayer gliding belt and the fault. Silication and pyritization widely exsist. There are obvious metallogenic regulation, and the result of metallogenic prognosis is satisfying.
Keywords:Dazhuangzi mining area  genetic type of gold deposits  metallogenic model  Guiding exploration
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