胶东西岭金矿床黄铁矿热电性特征及深部找矿意义
俞炳1,2,3,4(),丁正江1(),陈伟军5,李肖6,刘彩杰1,薛建玲3,4,曾庆栋7,8,范宏瑞7,8,吴金检7,8,张琪彬1
Thermoelectric Characteristics of Pyrite from the Xiling Gold Deposit in Jiaodong Peninsula and Its Implications for Deep Prospecting
Bing YU1,2,3,4(),Zhengjiang DING1(),Weijun CHEN5,Xiao LI6,Caijie LIU1,Jianling XUE3,4,Qingdong ZENG7,8,Hongrui FAN7,8,Jinjian WU7,8,Qibin ZHANG1

图1. 胶东金矿集区区域地质和主要金矿床分布图(修改自Fan et al.,2003
1.第四系沉积物;2.超高压变质岩;3.元古宙变质岩;4.太古宙变质岩(胶东群);5.早白垩世火山岩;6.早白垩世艾山花岗岩类;7.早白垩世郭家岭花岗闪长岩;8.晚侏罗世玲珑花岗岩类;9.晚三叠世花岗岩类;10.断裂;11.蚀变岩型金矿;12.石英脉型金矿

Fig.1. Regional geology and distribution map of main gold deposits in the Jiaodong gold Concentration area(modified after Fan et al.,2003