胶东西岭金矿床黄铁矿热电性特征及深部找矿意义
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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
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Thermoelectric Characteristics of Pyrite from the Xiling Gold Deposit in Jiaodong Peninsula and Its Implications for Deep Prospecting
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Bing YU 1,2,3,4( ),Zhengjiang DING 1( ),Weijun CHEN 5,Xiao LI 6,Caijie LIU 1,Jianling XUE 3,4,Qingdong ZENG 7,8,Hongrui FAN 7,8,Jinjian WU 7,8,Qibin ZHANG 1
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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
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Fig.1. Regional geology and distribution map of main gold deposits in the Jiaodong gold Concentration area(modified after Fan et al.,2003)
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