中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Distribution and controlling factors of nickel and cobalt in the Jinchuan magmatic Cu-Ni sulfide deposit.

文献类型:期刊论文

作者Yuan QingHan1,2; Su BenXun1,2
刊名ACTA PETROLOGICA SINICA
出版日期2023-04-01
卷号39期号:4页码:1030-1040
关键词Ni-Codistribution Oreminerals Gangue minerals Jinchuan Cu-Ni sulfide deposit
ISSN号1000-0569
DOI10.18654/1000.0569/2023.04.06
英文摘要Nickel(Ni)andcobalt(Co) havesimilargeochemicalbehaviorsduringtheformationandevolutionofthemantle. derivedmagmas.JinchuanmagmaticCu.NisulfidedepositcontainsNiandCuasthemaineconomiccommoditieswithCoasby. product.DespitethesimilarspatialdistributionofNiandCo,thecuriouslyhigherNi/Coratio(36.7) oftheJinchuandeposit comparedtothatofmantle(18.2)indicatestheparagenesisandseparationbetweenNiandCooccurredduringthemetallogenic processes,whosemechanism remainspoorlyunderstood.ThispapersummarizestheconcentrationsofNiandCooforeminerals comparingwithganguemineralsinordertogainabetterunderstandingofthedistributionofNiandCo,anditscontrollingfactors.The resultsshowthatthepentlanditeservesastheprimaryreservoirforNiandCo,withsubstantiallyhighercontentsthanpyrrhotite, chalcopyriteandthegangueminerals.Regardingthegangueminerals,olivinehasthehighestNicontentsfollowedbymagnetite, chromite,orthopyroxeneandclinopyroxene. Cobaltisrichestinchromitefollowedbyolivine,orthopyroxene,clinopyroxeneand magnetite.SinceNiismuchmorecompatibleinsulfideliquidsthanCoduringthesulfidesegregation,Nibecomessignificantly enrichedintheimmisciblesulfidemeltwhileCobecomesrelativelyenrichedinthesilicatemelt,resultinginthedecouplingofNiand Co.Duringthecrystallizationofsulfideliquids,bothNiandCotendtobeconcentratedtogetherintheearlycrystallizedMSS. Subsequently,pentlanditeexsolvedfromMSS,becomingthemostimportantreservoirofNiandCoandresultingthesimilarspatial distributionofNiandCo.Duringthedifferentiationofsilicateliquids,Niishighlycompatibleinolivine,whileCoishighlycompatible inchromite.Therefore,fractionalcrystallizationofcumulusolivineandchromiteintheJinchuandepositresultsinthedecouplingofNi andCo.Incontrast,thecrystallizationoforthopyroxeneandclinopyroxene,inwhichNiismorecompatiblethanCo,isbalancedbythe depletionofNiintheintercumulusresidualmelts.Thesub.solidusdiffusionofNiandCofromolivine,chromite,orthopyroxeneand clinopyroxeneintosulfideliquidsexertseffectsontheNi.Codistributioncompletelyoppositetocrystallization.Giventhatpentlandite andpyrrhotiteexsolvedfromMSScrystallizingfromsulfideliquidsatearlystage,thecovariantNiandCocontentsofthembetween differentrock/oretypesprovethatelementscompatiblewithMSSinpentlanditeandpyrrhotitecanbeusedtoindicatetheevolutionof sulfideliquids
WOS关键词OXYGEN FUGACITY ; TEMPERATURE ; OLIVINE ; SULFUR ; MELT
WOS研究方向Geology
语种英语
WOS记录号WOS:000970513600006
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/110880]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Su BenXun
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
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Yuan QingHan,Su BenXun. Distribution and controlling factors of nickel and cobalt in the Jinchuan magmatic Cu-Ni sulfide deposit.[J]. ACTA PETROLOGICA SINICA,2023,39(4):1030-1040.
APA Yuan QingHan,&Su BenXun.(2023).Distribution and controlling factors of nickel and cobalt in the Jinchuan magmatic Cu-Ni sulfide deposit..ACTA PETROLOGICA SINICA,39(4),1030-1040.
MLA Yuan QingHan,et al."Distribution and controlling factors of nickel and cobalt in the Jinchuan magmatic Cu-Ni sulfide deposit.".ACTA PETROLOGICA SINICA 39.4(2023):1030-1040.

入库方式: OAI收割

来源:地质与地球物理研究所

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