Serveur d'exploration sur le nickel au Maghreb

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

Identifieur interne : 001469 ( Main/Exploration ); précédent : 001468; suivant : 001470

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

Auteurs : Michael P. Foose [États-Unis] ; Maria Economou [Grèce] ; A. Panayiotou [Chypre (pays)]

Source :

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.

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DOI: 10.1007/BF00204279


Affiliations:


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