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新莲矿段海相火山岩型铜矿受地层岩性、构造、海相变基性火山岩控制,铜矿体赋存于老新街背斜轴部及其两翼变基性火岩中,变基性火山岩既是成矿母岩,也是容矿岩石,具有矿床规模大、品位稳定、矿体成带成群分布、矿石质量好的特点;通过前期整装勘查工作,总结出了“四旋回、六层楼”矿化模式,目前已探获铜资源量达中型矿床规模;对比75-127勘探线范围内已探获的铜资源量,预测新莲矿段矿床规模可达大型,铜资源量可达50万t以上。
The Xinlian ore section marine volcanic copper deposit is controlled by stratigraphic lithology, tectonism and marine facies basic volcanic rocks. The copper ore body exists in the shaft part of old Xinjie anticline and its metamorphic rock, The volcanic rocks are not only the host metallogenic rocks but also the ore-hosting rocks, which have the characteristics of large-scale deposit, stable grade, clustered distribution of ore bodies and good ore quality. Through the pre-installation survey, Six-storey "mineralization mode, and the copper resources have been explored to reach the scale of medium-sized deposits. Compared with the copper resources already explored in the area of 75-127 exploration lines, it is predicted that the ore scale of Xinlintuan ore section will reach a large scale and the copper resources The amount of up to 500000 t above.