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该矿系以银铅锌为主伴生金的多金属矿床,成矿受火山机构及断裂的控制,空间上、成因上与早白垩世超浅成石英斑岩有关。矿体分为铅锌矿及银铅锌矿两种,形态为似层状、薄层状及脉状,主要产在石英斑岩体的接触带附近,矿化以细脉浸染状为主,近矿围岩具有以硅化、绢云母化为主的面型蚀变,据此特点,初步认为矿床成因类型应属浅成、超浅成次火山斑岩型矿床。此一新型矿床的发现与认识的提出,旨在读者中引起反响,共同商权,欲对找矿与研究工作有所裨益。
The deposit is dominated by silver, lead and zinc polymetallic deposits. Its mineralization is controlled by volcanic structures and faults. It is spatially and genetically related to the Early Cretaceous ultra-shallow quartz porphyry. The ore body is divided into two kinds of lead-zinc ore and silver-lead-zinc ore, the shape is like stratified, lamellar and vein-shaped, mainly produced near the contact zone of quartz porphyry body, According to this feature, the type of ore deposits should be shallowly-supergene, super-shallow volcanic porphyry deposit. The discovery and recognition of this new type of deposit are intended to arouse repercussions among readers and to jointly exercise their rights and interests in the prospecting and research work.