CAJ | 학술논문

通过对新疆鄯善县红石金矿床野外调研、总结矿床地质特征,对该矿床钻孔中原生晕分布特征和规律进行了专题研究,采用多种计算方法相互印证,确立红石金矿床原生晕轴向分带序列为Bi-Me-Hg-zn-Pb-Ag-As-Cu-Sb-Au,同中国典型金矿床轴向分带序列对比,发现其具有逆向分带的特征,从而建立分带评价及矿体叠加模式,为深部隐伏矿预测提供依据.
통과대신강선선현홍석금광상야외조연、총결광상지질특정,대해광상찬공중원생훈분포특정화규률진행료전제연구,채용다충계산방법상호인증,학립홍석금광상원생훈축향분대서렬위Bi-Me-Hg-zn-Pb-Ag-As-Cu-Sb-Au,동중국전형금광상축향분대서렬대비,발현기구유역향분대적특정,종이건립분대평개급광체첩가모식,위심부은복광예측제공의거.
Based on field investigation of the Hongshi gold deposit and summarization of its geological features,the authors made a special study of the distribution characteristics and regularity of primary halos in this ore deposit by using different calculation methods, and found that the axial zoning sequence of the primary halos in the deposit is Bi-Mo-Hg-Zn-Pb-Ag-As-Cu-Sb-Au. A comparison with axial zoning sequences of other typical gold deposits in China reveals that the axial zoning sequence of primary halos in this ore deposit is obviously characterized by reversed zoning. The zoning evaluation model and the ore body superimposition pattern for this ore deposit were also set up so as to predict concealed ore bodies in the depth.