【摘 要】
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Hydrothermal cobalt deposits provide a valuable example in understanding the relationship between mafic magmatism and mineralization.Three main types of hydroth
【机 构】
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Institute of Geology and Mineralogy,IGM,SB RAS,
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Hydrothermal cobalt deposits provide a valuable example in understanding the relationship between mafic magmatism and mineralization.Three main types of hydrothermal cobalt ore deposits have been recognized in the Altay-Sayan fold belt(Russia), which are Ni-Co-arsenic(Ni-Co-As),Co-sulfoarsenic (Co-As),and Cu-Co-sulfoarsenic-sulfosaltic(Cu-Co -As).Cobalt mineralization in this district is characterized by well zonation,commonly with the following sequence:Co-sulfoarsenic ores in metasomatic rocks→Ni-Co-As mineralization in carbonate veins→Cu-Co-sulfoarsenic-sulfosalts
Hydrothermal cobalt deposits provide a valuable example in understanding the relationship between mafic magmatism and mineralization. Three major types of hydrothermal cobalt ore deposits have been recognized in the Altay-Sayan fold belt (Russia), which are Ni-Co-arsenic (Ni-Co Co-sulfoarsenic (Co-As), and Cu-Co-sulfoarsenic-sulfosaltic (Cu-Co-As) .Cobalt mineralization in this district is characterized by well zonation, commonly with the following sequence: Co-sulfoarsenicores in metasomatic rocks → Ni-Co-As mineralization in carbonate veins → Cu-Co-sulfoarsenic-sulfosalts
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