Occurrence State and Ore-forming Regularity of Critical Metal Cobalt in the Changsha-Pingjiang Fault Zone,Northeastern Hunan Province
Received date: 2020-08-07
Revised date: 2020-09-14
Online published: 2021-01-29
Recently,the exploration of cobalt resources in the Jingchong-Beishan area,the east of Changsha-Pingjiang fault zone,northeastern Hunan Province,has made great advances.Some Co (-polymetallic) vein deposits including the medium-size Jingchong Cu-Co polymetallic deposit and Hengdong Co-Cu deposit,and Dayan Au-Co occurrence were discovered in this region.Based on the detailed field observation,this study identified the ore stages,and concluded the metallogenic characteristics of Changsha-Pingjiang cobalt ore belt as well as the ore-forming factors.The combined microscopic observation and in-situ analytical methods revealed that the metal Co was mainly incorporated in fine-grained pyrite and arsenopyrite as stoichiometric substitution,with subordinate occurrence as independent mineral cobaltite.The complicated texture and chemical compositions of Co-beating pyrite and arsenopyrite indicated that pyrite associated with arsenopyrite has the higher Co concentration (up to 13.48%),greater than that in arsenopyrite-exclusive assemblages.Therefore,the mineral assemblage of fine-grained pyrite and arsenopyrite can be used as the mineral fingerprint to trace the high-grade Co ores during the prospecting exploration.Subsequently,the preliminary mineral processing technology was proposed.
Zhilin WANG , Yang WU , Deru XU , Shaohao ZOU , Guojun DONG , Erke PENG , Juntao NING , Bo KANG . Occurrence State and Ore-forming Regularity of Critical Metal Cobalt in the Changsha-Pingjiang Fault Zone,Northeastern Hunan Province[J]. Gold Science and Technology, 2020 , 28(6) : 779 -785 . DOI: 10.11872/j.issn.1005-2518.2020.06.147
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