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许多金属、非金属矿床的形成是与缺氧环境有关的成矿作用及其区域和全球背景耦合的结果 .两者相互作用并长期谐同和持续发展控制了矿床的大、超大规模 .建立了 3种缺氧环境成矿作用模式 ,确定了 3类重要的背景型式 .地史上的重大转折期是大、超大矿床形成的有利时期 .
The formation of many metallogenic and nonmetallic deposits is the result of metallogenetic interactions related to anoxic environments and their regional and global background coupling.The interaction and long-term harmonization and sustainable development control the large-scale and ultra-large-scale mineral deposits.The paper establishes 3 Three types of important background patterns have been identified for the mineralization mode of anoxic environments, and the significant turning point in the history of the earth is the favorable period for the formation of large and superlarge deposits.