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《Journal of Changchun University of Science and Technology》 2001-01
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DAHENGLU TYPE OF COBALT DEPOSIT IN LAOLING AREA,JILIN PROVINCEA SEDEX DEPOSIT WITH LATE REFORMATION

YANG Yan_chen, FENG Ben_zhi, LIU Peng_e (College of Earth Sciences, Jilin University ,Changchun 130026,China)  
Existing in Laoling metallogenic zone of gold and polymetallic deposits, Dahenglu type cobalt deposit is a newly found new type deposit,which is located in the middle section of Liaoji Proterozoic rifting zone This type deposit is formed in the formation of B-rich and C-rich phyllite with quartzite (siliceous rocks) as intercalated beds,which belongs to early Proterozoic Laoling group;the orebodies are composed of C-bearing sericite phyllite,tourmaline-bearing sericite phyllite,quartzite and tourmalite,and existed in the forms of bed and saddle whose occurances concordant with wall rocks The author find that the cobalt in ore is in the form of indepent minerals,such as siegenite,cobaltite, skutterudite and Co-bearing pyrite etc Studies on the aspects of strata bound characteristics,occurances of orebodies,sedimentary fabrics of ore,geochemistry of ore-bearing rocks,hot water sedimentary rocks,rare earth elements and isotope etc,indicate that this deposit has obvious genetic characteristics of submarine hot water desposition and was intensely refouned by later thermal solutions Based on all the above said the author suggests Dahenglu type cobalt deposit has genesis of submarine hot water deposition,superimposed by late thermal solutions
【Fund】: 原地质矿产部定向基金资助项目 !( 96 - 0 7);; 高等学校博士点基金资助项目! ( 941870 3)
【CateGory Index】: P618.62
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