青海省南祁连阳康地区水系沉积物地球化学特征及成矿远景

    GEOCHEMICAL CHARACTERISTICS AND METALLOGENIC PROSPECT OF STREAM SEDIMENTS IN YANGKANG AREA ON THE SOUTHERN SIDE OF QILIAN MOUNTAINS

    • 摘要: 阳康地区位于南祁连加里东期钨-锡-金-铜成矿带哈拉湖-龙门加里东期钨-金-铜-钴成矿亚带, 成矿带内已发现金属矿床(点)几十处, 具有良好的多金属找矿前景. 区内已发现多金属矿(化)点共5处. 通过开展1:5万水系沉积物测量, 对区内20种元素原始数据进行分析, 其中Au、As、Sb、W、Pb、Zn等10种元素丰度值高于全区, 尤其是在志留系巴龙贡嘎尔组变质砂岩中呈现强富集. 初步统计分析了水系沉积物富集系数、变异系数, 其中Au元素富集系数K=2.14, Au、Pb、W元素变异系数较大. 通过对样品进行R型聚类分析, 划分为4个亚簇: Ⅱ-1簇As-Sb-Mo、Ⅱ-2簇Bi-Sn-Rb-U、Ⅱ-3簇Ba、Ⅱ-4簇Ag-Pb. 圈定出综合异常48处, 分类排序后选定代表性和找矿前景较好的2处甲类和2处乙类异常特征进行重点评述. 依据元素分布特征、元素相关性、综合异常特征, 结合区域地质成矿背景, 划分出3个成矿远景区, 分别为Ⅱ级色热多陇金钨成矿远景区、多尔盖铅锌成矿远景区和Ⅲ级拉木龙钨铜金成矿远景区.

       

      Abstract: Yangkang area is located in the Hala Lake-Longmen Caledonian W-Au-Cu-Co metallogenic subbelt of Caledonian W-Sn-Au-Cu metallogenic belt on the southern side of Qilian Mountains, with dozens of metal deposits (occurrences) found in the metallogenic belt, which has a good polymetallic exploration prospect. A total of 5 polymetallic mineral occurrences or mineralization spots have been found in the area. Through the 1:50 000 stream sediment survey, the primary data of 20 elements in the area are analyzed, among which the abundances of 10 elements such as Au, As, Sb, W, Pb and Zn are higher than the average of the region, especially highly enriched in the metamorphic sandstone of Silurian Balonggar Formation. The statistical analysis of stream sediments shows that the enrichment coefficient (K) of Au is 2.14, with great variation coefficients of Au, Pb and W. The samples are classified into 4 subclusters by R-type cluster analysis, i.e. Ⅱ-1 of As-Sb-Mo, Ⅱ-2 of Bi-Sn-Rb-U, Ⅱ-3 of Ba and Ⅱ-4 of Ag-Pb. From the 48 delineated comprehensive anomalies, 2 of Class A and 2 of Class B anomalies with good representativeness and exploration prospects are selected for emphasis discussion. According to the element distribution, element correlation and comprehensive anomaly characteristics, combined with the regional metallogenic background, 3 metallogenic prospect areas are defined, namely the second-order Sereduolong Au-W metallogenic prospect area, second-order Duoergai Pb-Zn metallogenic prospect area and third-order Lamulong W-Cu-Au metallogenic prospect area.

       

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