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普朗铜矿床位于西南三江地区格咱弧东斑(玢)带,与印支期普朗复式中酸性斑(玢)岩体有关,是该区发现的最大规模的铜矿床。对于斑岩型铜矿床来说,其成矿地质体主要为侵入岩体,是形成矿体(床)成矿地质作用的实物载体,成矿作用主要集中于岩浆房高位突出的小岩体顶部及其内外接触带范围内,在预测工作中,利用其和矿床(体)的确定性关系就可以明确找矿方向。特别对于普朗超大型铜多金属矿床来说,如此规模的金属是如何聚集并沉淀的,什么样的成矿地质体可以带来这么多的金属元素,还或者是
The Pulang copper deposit is located in the southern part of the Geze arc eastern Sanjiang area (玢) belt, which is related to the Indosinian Plankian intermediate-acidic patch (玢) rock mass and is the largest copper deposit discovered in the area. For the porphyry-type copper deposits, the metallogenic geology is mainly intruded into the rock mass, which is a physical carrier that forms the ore-forming geological function of the orebody (bed). The mineralization mainly concentrates in the small rock mass protruding from the top of the magma chamber Top and within the contact zone with its inside and outside the scope of the forecasting work, the use of its relationship with the deposit (body) can determine the direction of prospecting. Especially for the Pulang super-large copper-polymetallic deposits, how such metals are aggregated and precipitated, what kind of metallogenic geology can bring so many metal elements, or