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夹皮沟金矿田北沟金矿床原生晕特征及深部成矿预测

Primary halo characteristics and deep metallogenic prediction of Beigou Gold Deposit in Jiapigou Gold Field

  • 摘要: 北?到鹂蟠参挥诩衅す到鹂筇锉辈浚衅す当蔽飨蚬乖焓幢浯卸巍1惫到鹂笄诳筇甯炒嬗诩衅す等浩檠抑校笫允⒙鲂秃褪⑼鲂臀鳌Mü钥蟠驳刂侍卣鳌⒖笫卣骷霸蔚厍蚧卣鞯难芯浚衔鹂蠡爰衅す等浩檠摇⒓刂驶ǜ谘姨濉⒅猩兴嵝月鲅夜叵得芮校槐蔽飨蚬乖焓幢浯潜惫到鹂蟠仓饕乜蠊乖臁T畏治鼋峁砻鳎惫到鹂蟠部筇宓脑卮瓜蚍执蛄形As-Hg-Sb-Ag-Pb-Cu-Te-Au-S-Bi-Zn-Ni-Co-Mo-W-Mn。通过对北沟金矿床元素垂向分带模式的分析,结合前缘晕元素Hg异常浓聚中心到矿体头部距离是240 m,预测在深部1 050 m处存在矿体。通过与已有钻孔信息进行对比,该处已发现矿体,与本次预测结果一致。

     

    Abstract: Beige Gold Deposit is located in the north of Jiapigou Gold Field and  in the middle of the NW-trending structural alteration zone of Jiapigou.The ore body occurs in gneisses of Jiapigou group,and the ores are mainly quartz vein type and quartz stockwork type.Based on the study of geological characteristics,ore characteristics and primary halo geochemical characteristics of the deposit,it is considered that gold mineralization is closely related to gneisses of Jiapigou group,potassic granites,and Mesozoic intermediate-acid dykes.The NW-trending structural alteration zone is the main ore-controlling structure of Beigou Gold Deposit.The results of primary halo analysis show that the longitudinal vertical zonation sequence of the Beigou Gold Deposit is As-Hg-Sb-Ag-Pb-Cu-Te-Au-S-Bi-Zn-Ni-Co-Mo-W-Mn.Based on the analysis of vertical geochemical zonation pattern of element in Beigou Gold Deposit,and the fact that the distance from the abnormal center of frontal halo elements Hg to the head of the ore body is 240 m,it is predicted that the ore body should be at the depth of 1 050 m.Through the comparison of the existing drilling information,the ore body has been found,which is consistent with the prediction results.

     

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