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本文以湘南铜山岭多金属矿床为实例,论述了斑岩、夕卡岩、热液、层控四类矿床之间不仅在成因上有着内在联系,而且在空间上也可出现共生规律。从而提出斑岩—夕卡岩—热液—层控多因共生成矿模式。并认为这种模式的建立有助于把成矿研究从单一成因论引向多因共生,多因复成及成矿系列的概念,并在实用上有助于找矿勘探中开拓新的思路。
In this paper, taking the Tongshanling polymetallic deposit in southern Hunan as an example, this paper discusses that the four types of deposits of porphyry, skarn, hydrothermal and stratabound are not only intrinsically linked but also spatially coexistent. Thus proposed porphyry - skarn - hydrothermal - strata multi-genesis co-mineralization mode. It is also believed that the establishment of this model will help to direct the study of metallogenesis from single genesis to the concept of multi-symbiosis, multi-genesis and metallogenic series and help to open up new ideas in prospecting. .