摘要
Any of iron-copper ore deposits, without exception, contains various associated components. The studies on the distribution and mode of occurrence of over 20 associated elements in 87 iron-copper ore deposits in a certain district in China have shown that the specificity of the associated element distribution is eontrolled by the type of the deposits, that there exists a close relation between ore.forming and associated elements, and that the formation conditions and type of ore deposits, and the geochemical properties of the elements are the decisive factors governing the migration and enrichment of the associated elements during minerogenetie process.
Any of iron-copper ore deposits, without exception, contains various associatedcomponents. The studies on the distribution and mode of occurrence of over 20associated elements in 87 iron-copper ore deposits in a certain district in China haveshown that the specificity of the associated element distribution is controlled bythe type of the deposits, that there exists a close relation between ore-forming andassociated elements, and that the formation conditions and type of ore deposits, andthe geochemical properties of the elements are the decisive factors governing the mig-ration and enrichment of the associated elements during minerogenetic process.
出处
《地球化学》
CAS
1975年第4期235-249,共15页
Geochimica