NickelMaghrebV1, Istex, Corpus, bibRecord, 000507

Compositional and mineralogic constraints on the genesis of ophiolite hosted nickel mineralization in the Pevkos area, Limassol Forest, Cyprus

Identifieur interne : 000507 ( Istex/Corpus ); précédent : 000506; suivant : 000508

Compositional and mineralogic constraints on the genesis of ophiolite hosted nickel mineralization in the Pevkos area, Limassol Forest, Cyprus

Auteurs : Michael P. Foose ; Maria Economou ; A. Panayiotou

Source :

Mineralium Deposita [ 0026-4598 ] ; 1985-10-01.

RBID : ISTEX:8FE8C2E66B92F40DEA0D26324B4903717234F0C7

Abstract

Abstract: Mineralization composed dominantly of primary troilite, maucherite, pentlandite, and chalcopyrite, and secondary valleriite occurs in serpentinized transition zone rocks of the Limasol Forest segment of the Troodos ophiolite complex, Cyprus. Whole-rock and electron microprobe analyses of this mineralization gives ranges of Cu/(Cu+Ni)=0.16 to 0.47, Pt/(Pt+Pd)=0.66 to 0.51, Ni/Co=6.33 to 13.4, and chondrite normalized plots with low concentrations of Rh, Pt, and Pd, but relatively high Au. Estimated distribution coefficients of nickel and iron between olivine and ore range from 0.5 to 7.4. Most of these data are unlike values from magmatic sulfide deposits and indicate either a complete alteration of a preexisting magmatic sulfide concentration or, more likely, a nonmagmatic origin for this mineralization.

Url:

https://api.istex.fr/document/8FE8C2E66B92F40DEA0D26324B4903717234F0C7/fulltext/pdf

DOI: 10.1007/BF00204279

Links to Exploration step

ISTEX:8FE8C2E66B92F40DEA0D26324B4903717234F0C7

Le document en format XML

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<abstract lang="en">Abstract: Mineralization composed dominantly of primary troilite, maucherite, pentlandite, and chalcopyrite, and secondary valleriite occurs in serpentinized transition zone rocks of the Limasol Forest segment of the Troodos ophiolite complex, Cyprus. Whole-rock and electron microprobe analyses of this mineralization gives ranges of Cu/(Cu+Ni)=0.16 to 0.47, Pt/(Pt+Pd)=0.66 to 0.51, Ni/Co=6.33 to 13.4, and chondrite normalized plots with low concentrations of Rh, Pt, and Pd, but relatively high Au. Estimated distribution coefficients of nickel and iron between olivine and ore range from 0.5 to 7.4. Most of these data are unlike values from magmatic sulfide deposits and indicate either a complete alteration of a preexisting magmatic sulfide concentration or, more likely, a nonmagmatic origin for this mineralization.</abstract>
<relatedItem type="host"><titleInfo><title>Mineralium Deposita</title>
<subTitle>International Journal of Geology, Mineralogy and Geochemistry of Mineral Deposits</subTitle>
</titleInfo>
<titleInfo type="abbreviated"><title>Mineral. Deposita</title>
</titleInfo>
<genre type="journal" displayLabel="Archive Journal"></genre>
<originInfo><dateIssued encoding="w3cdtf">1985-10-01</dateIssued>
<copyrightDate encoding="w3cdtf">1985</copyrightDate>
</originInfo>
<subject><genre>Geosciences</genre>
<topic>Geology</topic>
<topic>Mineral Resources</topic>
<topic>Mineralogy</topic>
</subject>
<identifier type="ISSN">0026-4598</identifier>
<identifier type="eISSN">1432-1866</identifier>
<identifier type="JournalID">126</identifier>
<identifier type="IssueArticleCount">16</identifier>
<identifier type="VolumeIssueCount">4</identifier>
<part><date>1985</date>
<detail type="volume"><number>20</number>
<caption>vol.</caption>
</detail>
<detail type="issue"><number>4</number>
<caption>no.</caption>
</detail>
<extent unit="pages"><start>234</start>
<end>240</end>
</extent>
</part>
<recordInfo><recordOrigin>Springer-Verlag, 1985</recordOrigin>
</recordInfo>
</relatedItem>
<identifier type="istex">8FE8C2E66B92F40DEA0D26324B4903717234F0C7</identifier>
<identifier type="DOI">10.1007/BF00204279</identifier>
<identifier type="ArticleID">BF00204279</identifier>
<identifier type="ArticleID">Art2</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1985</accessCondition>
<recordInfo><recordContentSource>SPRINGER</recordContentSource>
<recordOrigin>Springer-Verlag, 1985</recordOrigin>
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<serie></serie>
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Compositional and mineralogic constraints on the genesis of ophiolite hosted nickel mineralization in the Pevkos area, Limassol Forest, Cyprus

Compositional and mineralogic constraints on the genesis of ophiolite hosted nickel mineralization in the Pevkos area, Limassol Forest, Cyprus

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