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只是在最近才逐渐查明热液-沉积硫化物的成矿作用在内生金属矿床成因中所起的作用。自从C.Ofsedahl(1958)和В.И.Смирнов(1960)首次把主要组成黄铁矿矿床的硫化物矿石划分为同生沉积成因以来,这种矿石日益引起广大地质界的注意并对它们进行了系统的研究。Н.С.Скрипченко(1963)首先注意到热液-沉积成矿作用与交代成矿作用在地球化学上的根本区别。后来,由于В.И.Смирнов
Only recently has it been gradually ascertained that the mineralization of hydrothermal-sedimentary sulphides plays a role in the genesis of endogenous metallogenic deposits. Since C.Ofsedahl (1958) and В.И.Смирнов (1960) have for the first time classified sulphide ores, which are mainly composed of pyrite deposits, into syn-sedimentary origin, such ores have increasingly attracted the attention of the vast geological community and have been subjected to them The systematic research. Н.С.Скрипченко (1963) first noticed the fundamental geochemical difference between hydrothermal-sedimentary mineralization and metasomatism. Later, due to В.И.Смирнов