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在对华南武夷-云开地区铜铅锌金(银)矿床成因类型划分的基础上,扼要讨论了各类型矿床时空的分布规律,指出区内与岩浆作用有关的铜铅锌金(银)矿床主要形成于燕山期,并细分为燕山期早、晚两个阶段,两阶段金属矿床的分布范围和控岩控矿构造条件是不同的;与沉积作用有关的铅锌(银)矿床绝大多数分布于晚古生代张裂盆地内,受泥盆系和石炭系一定层位控制,其成因与同生热水沉积作用有关.文章最后划分和建立了该地区铜铅锌(金银)矿床的区域成矿系列和矿床成矿系列.
Based on the genetic type classification of Cu-Pb-Zn-Au (Ag) deposits in Wuyi-Yunkai area in South China, the temporal and spatial distribution of various types of deposits is briefly discussed. It is pointed out that the Cu-Pb-Zn- Mainly formed in the Yanshanian period and subdivided into two phases of early and late Yanshanian period. The distribution range of the two-stage metallogenic deposits is different from that of the controlled ore-controlling structure; the lead-zinc (silver) deposit related to sedimentation is extremely large Mostly distributed in the late Paleozoic rift basin and controlled by a certain horizon of Devonian and Carboniferous, the genesis is related to syngenetic hydrothermal deposition.At the end of this article, the copper, lead, zinc (gold, silver) deposit Regional metallogenic series and metallogenic series of deposits.