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矿床成因一直是从事矿床工作的生产、教学和科研人员共同关注的重要问题.长期以来,可以说自从矿床学开始萌芽以来,无论对矿床成因持何种观点,内生或外生、岩浆或冷水,一般都是单一的成因论者.只有对少数矿床,如某些沉积变质矿床、沉积-浅变质-风化壳型富铁矿床等,才认为不同的、相隔时间很长久的地质作用在成矿全过程中都很重要,即这些矿床是多成因的.过去,对大多数矿床持单一成因观点,这是不足为奇的.我们在野外看到的只是长
The origin of the deposit has always been an important issue that the production, teaching and research personnel engaged in the deposit work have always been concerned with.For a long time, it can be said that since the mineralization began to sprout, no matter what the origin of the deposit, whether endogenous or exogenous, magmatic or cold , Are generally single cause of genesis.Only a small number of deposits, such as some sedimentary metamorphic deposits, sedimentary - metamorphic - weathered crust-rich iron ore deposits, etc., that different, long time interval geology in the The whole process of the mine is very important, that is, these deposits are multi-genesis. In the past, it is not surprising that most of the deposits hold the same genesis perspective.