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热液中矿物质迁移条件和形式的实验研究及理论解释是矿石建造成因模式的一个重要方面.一般来说,天然热液为高度浓缩的真溶液,它以氯化物、氟化物、碳酸盐、硫化物、硫氢化物络合物和羟基化物形式携带溶质.至于这些物质的迁移,多数人认为与羟基氯化物或羟基氟化物型混合络合物的形成有关,或者与各种同多酸的衍生物有关.同时,根据含矿流体的还原性和在矿物流体包裹体中发现有机化合物的事实,也有人认为矿物质是以元素的有机化合物形式迁移的.
Experimental study and theoretical interpretation of mineral migration conditions and forms in hydrothermal fluids is an important aspect of the genetic model of ore formation. In general, natural hydrothermal fluids are highly concentrated, true solutions in the form of chlorides, fluorides, carbonates , Sulfides, hydrosulfide complexes, and hydroxylates As far as the migration of these materials is concerned, most are thought to be involved in the formation of mixed complexes of hydroxychlorohydrochloride or hydroxyfluoride type or with various polyacid At the same time, according to the reducibility of ore-bearing fluids and the fact that organic compounds are found in mineral fluid inclusions, it is also thought that minerals migrate as elemental organic compounds.