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金属矿山 ›› 2025, Vol. 54 ›› Issue (9): 240-251.

• 地质与测量 • 上一篇    下一篇

鄂东南鸡冠咀铜金矿钻孔原生晕地球化学特征及成矿预测

程孝增1   刘冬勤2   朱  金1   秦志军1   张小波1   周润杰1   熊意林1     蔡恒安3   尚世超3   周  豹1    

  1. 1. 湖北省地质调查院,湖北 武汉 430034;2. 湖北省地质局第八地质大队,湖北 襄阳 441002; 3. 湖北省地质局第一地质大队,湖北 大冶 435100
  • 出版日期:2025-09-15 发布日期:2025-10-10
  • 通讯作者: 周  豹(1985—),男,高级工程师,硕士。
  • 作者简介:程孝增(1992—),男,工程师,硕士。
  • 基金资助:
    中国地质调查局专项(编号:1212011220701);湖北省自然科学基金项目(编号:2023AFD213)。 

Geochemical Characteristics of Primary Halo and Deep Metallogenic Prognosis of Jiguanzui Cu-Au Deposit in Daye,Hubei Province 

CHENG Xiaozeng 1   LIU Dongqin 2   ZHU Jin 1   QIN Zhijun 1   ZHANG Xiaobo 1   ZHOU Runjie 1      XIONG Yilin 1   CAI Heng′an 3   SHANG Shichao 3   ZHOU Bao 1    

  1. 1. Hubei Geological Survey,Wuhan 430034,China;2. The Eighth Geological Brigade of Hubei Geological Bureau, Xiangyang 441002,China;3. The First Geological Brigade of Hubei Geological Bureau,Daye 435100,China
  • Online:2025-09-15 Published:2025-10-10

摘要: 鸡冠咀铜金矿床位于我国重要的长江中下游 Cu-Fe-Au-Mo 矿产聚集带鄂东南矿集区内,矿体以脉状、 薄板状为主,矿床受断裂—接触带构造、大理岩内的雁状裂隙控制,属岩浆期后高—中温气液型铜金矿床。 以鸡冠咀 铜金矿Ⅶ#矿体 28 #勘探线剖面中的 8 个钻孔 927 件样品原生晕数据为研究对象,利用因子分析、相关性分析、聚类分 析对矿体元素亲疏程度进行了研究,采用格里戈良分带指数法确定了原生晕的轴向分带序列,并结合原生晕异常特 征、原生晕地球化学参数特征等对Ⅶ#矿体边深部隐伏矿体进行了成矿预测。 研究结果表明:① Au、Cu、Co、W、Mo 之 间相关性较大,Au、Cu、Ag、Zn、Pb 是成矿最直接的指示元素。 ② 矿体原生晕轴向分带序列为 As-Sb-W-Co-Au-CuAg-Ni-Pb-Zn;前缘晕 As、Sb 和尾晕 W、Mo 共存,尾晕元素 Ni 出现在近矿指示元素 Pb、Zn 上部,指示矿体是多期次叠 加而成,矿体在轴向上向两侧边界有延伸的可能。 ③ w(Sb) / w(W)、w(As+Sb) / w(W+Ni)所反映的前缘晕与尾晕元 素比值在边界处较大,且有增加趋势,同样指示矿体沿轴向上有向两侧延伸的可能。 综合分析认为:鸡冠咀 28 #线Ⅶ# 矿体在剖面两侧仍有成矿的条件及趋势,有必要进行进一步工程验证。 

关键词: 原生晕  地球化学特征  鸡冠咀铜金矿  成矿预测

Abstract: The Jiguanzui Cu-Au Deposit is located in the southeastern part of Hubei Province,an important Cu-Fe-AuMo mineral accumulation zone in the middle and lower reaches of the Yangtze River in China. The orebody is mainly in the form of veins and thin plates,and the deposit is controlled by the fault contact zone structure and the goose shaped fractures in the marble. It belongs to the high to medium temperature gas-liquid type copper gold deposit after the magmatic period. Taking 927 pieces of primary halo data from 8 boreholes in No. 28 exploration line profile of No. Ⅶ Cu-Au deposit in Jiguanzui as the study object,factor analysis,correlation analysis,and cluster analysis were used to study the degree of element affinity in the deposit. The Grigoryan zoning index method was adopted to determine the axial zoning sequence of the primary halo,and combined with the abnormal characteristics of the primary halo and the geochemical parameters of the primary halo,mineralization prediction was made for the hidden ore body in the deep edge of No. Ⅶ deposit. Research has shown that:① There is a strong correlation between Au,Cu,Co,W,and Mo,and Au,Cu,Ag,Zn,and Pb are the most direct indicator elements for mineralization. ② The axial zoning sequence of the primary halo of the ore body is As-Sb-W-Co-Au-Ag-Ni-Pb-Zn. The leading edge halos As and Sb coexist with the trailing edge halos W and Mo,and the trailing edge element Ni appears in the upper part of the near ore indicator elements Pb and Zn. The indicator orebody is formed by the superposition of multiple phases,and there is a possibility for the orebody to extend towards the two side boundaries in the axial direction. ③ The ratio of elements in the leading edge halo and tail halo reflected by w(Sb) / w(W) and w(As+Sb) / w(W+Ni) are relatively large at the boundary and shows an increasing trend,indicating the possibility of the orebody extending along the axial direction to both sides. Based on comprehensive analysis,it is believed that there are still mineralization conditions and trends on both sides of the section of No. Ⅶ orebody on No. 28 line of Jiguanzui,and further engineering verification is necessary. 

Key words: primary halo,geochemistry,Jiguanzui Cu-Au skarn deposit,metallogenic prediction 

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