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关于以碳酸盐岩石为容矿岩石的层控铅锌矿床的成因众说纷纭,莫衷一是。而对于这种矿床与沉积相的关系则谈论得很少。西班牙南部阿尔普贾里德阿尔卑斯三叠系中层控F—(Pb—Zn)矿床的地质特征表明,这些矿床明显地属于浅水相,其产状受泻湖环境中一定的相组合控制。一、阿尔普贾里德杂岩三叠系中层控F-(Pb-Zn)矿床的地质情况
There are different opinions on the causes of the stratabound lead-zinc deposit that uses carbonate rock as the ore-hosting rock. There is very little talk about the relationship between this deposit and the sedimentary facies. The geological features of the Triassic Middle Triassic F- (Pb-Zn) deposits in the Alpujration Alps in southern Spain indicate that these deposits clearly belong to the shallow water phase and their occurrences are controlled by a combination of phases in the lagoon environment. I. Geology of Triassic Middle-Controlled F- (Pb-Zn) Deposits in Alpujarid Complex