孙德君. 黑龙江省东部梧桐河—都鲁河流域流水成因砂金矿特点[J]. 地质与资源, 1992, 1(4): 228-234.
    引用本文: 孙德君. 黑龙江省东部梧桐河—都鲁河流域流水成因砂金矿特点[J]. 地质与资源, 1992, 1(4): 228-234.
    Shun Dejun. ALLUVIAL GOLD PLACER IN WUTONGHE-DULUHE DRAINAGE AREA OF EASTERN HEILONGJIANG PROVINCE[J]. Geology and Resources, 1992, 1(4): 228-234.
    Citation: Shun Dejun. ALLUVIAL GOLD PLACER IN WUTONGHE-DULUHE DRAINAGE AREA OF EASTERN HEILONGJIANG PROVINCE[J]. Geology and Resources, 1992, 1(4): 228-234.

    黑龙江省东部梧桐河—都鲁河流域流水成因砂金矿特点

    ALLUVIAL GOLD PLACER IN WUTONGHE-DULUHE DRAINAGE AREA OF EASTERN HEILONGJIANG PROVINCE

    • 摘要: 梧桐河-都鲁河流域是我国主要砂金富集区之一.区内以流水成因河漫滩砂金矿和阶地砂金矿为主.砂金矿的分布,明显地受矿质来源、新构造运动、水动力条件和沉积环境的控制.砂金矿体多呈带状、条带状赋存于河谷堆积物的底部,在矿体中经常出现一至几个富矿地段.砂金粒度为0.03-3.5mm.区内砂金矿的找矿前景好,主要找矿标志是旧采金迹、金矿化异常区和老变质岩分布区.根据砂金矿的分布和富集规律,可在五号山、小梧桐河北支沟、西梧桐河二支沟一带寻找岩金矿.

       

      Abstract: Wutonghe-Duluhe drainage area is one of the major concentration area of gold placers in China. In this area, the metamorphic rock series of Lower Proterozoic Heilongjiang group, Mashan group and Cretaceous volcanic rocks are widespread, Late Proterozoic migmatitic granite and Variscan granite cover a large area and Yanshanian granite, granitic-porphyry are mostly small stock. are S-N faults the major structures in this area and NE- and NW-trending faults are also developed and charactreistic of muitiple activity. This area is a low mountain-hilly geomorphic country with dendritic drainage of Wutonghe-Duluhe river system.

       

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