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柴窝堡铜矿区的层状铜矿属层间水压角砾岩控制的铜矿 ,脉状铜矿属高角度水力断裂控制的铜矿。首次在杏树沟发现产于石英钠长斑岩脉中的铜矿 ,并鉴别出铜沟控制Ⅰ号矿体的成矿构造为热泉通道。上述 4类成矿构造分属岩浆成矿构造系列与水压成矿构造系列。建立的成矿构造模式表明深部具有很好的找铜前景。
The stratiform copper deposit in the Chaiwopu copper deposit belongs to the copper deposit controlled by the interlayer hydraulic breccia, and the vein copper deposit is a copper deposit controlled by the high-angle hydraulic fracturing. For the first time in Xingshugou discovered in copper quartzite porphyry copper deposits, and identified the copper ditch control Ⅰ ore body ore structure for the hot spring channel. The above four types of metallogenic structures belong to series of magmatic mineralization and hydrothermal metallogeny series. The established metallogenic tectonic model indicates that the deep area has a good copper prospect.