Sulphur isotope study of Ni-Fe-Cu mineralization in the Shetland ophiolite

Hdl Handle:
http://hdl.handle.net/10149/98640
Title:
Sulphur isotope study of Ni-Fe-Cu mineralization in the Shetland ophiolite
Authors:
Maynard, J. B. (Jon); Prichard, H. M. (Hazel); Ixer, R. A. F. (Rob); Lord, R. A. (Richard); Wright, I. P. (Ian); Pillinger, C. (Colin); McConville, P.; Boyce, A. J. (Adrian); Fallick, A. (Anthony)
Affiliation:
University of Sunderland
Citation:
Maynard, J. et. al. (1997) 'Sulphur isotope study of Ni-Fe-Cu mineralization in the Shetland ophiolite', Transactions of the Institutions of Mining and Metallurgy, Section B: Applied Earth Science, 106 (Sept-Dec), pp.B215-B226.
Publisher:
Maney Publishing
Journal:
Transactions of the Institutions of Mining and Metallurgy, Section B: Applied Earth Science
Issue Date:
Sep-1997
URI:
http://hdl.handle.net/10149/98640
Abstract:
Sulphur isotope analyses of 62 samples from the Shetland ophiolite, Scotland, show that the sulphides throughout the igneous stratigraphy have a magmatic signature with the exception of the uppermost gabbros and the lowermost basal thrust talc-carbonate lithologies. Mean δ34S values for whole-rock samples from harzburgite (+3.5‰), dunite pods in harzburgite (+4.3‰), crustal dunite and wehrlite units (+2.5‰), the main pyroxenite unit (+2.9‰), the high-level pyroxenite (+4.1‰) and gabbro (+4.3‰) suggest that the primary sulphides derived their sulphur from a magmatic source enriched in 34S, which is compatible with the supra-subduction zone origin proposed for the Shetland ophiolite. δ34S values for pyrite mineralization in a gabbro, amphibole pegmatite and plagiogranite from the uppermost part of the gabbros range from +9.6 to +14.0‰ and are thought to result from precipitation from a 34S-enriched fluid, which, by analogy with other studies of ophiolitic crust, could have been derived from sea-water sulphate. A sulphide-bearing dunite from a dunite pod in mantle harzburgite at the Cliff locality that contains 4 ppm ∑Pt + Pd has an average δ34S value of +4.2‰, indistinguishable from values from other non-mineralized dunites from dunite pods and indicating a magmatic origin for this sulphur. In contrast, talc-carbonate altered rocks from the basal thrust, including samples from close to the Cliff locality, have an anomalously low mean δ34S value of +0.8‰, which can be explained by introduction of a proportion of isotopically light sulphur from the underlying metasedimentary sequence, which has a mean δ34S of -4.2‰. Stepped combustion analysis supports mineralogical observations that the majority of the sulphur is contained in disseminated Ni, Fe and Cu sulphides. δ34S laser probe data for intergrown pentlandite and heazlewoodite from the crustal dunite unit are essentially identical, which supports the idea that the replacement of pentlandite by heazlewoodite during serpentinization is isochemical with respect to sulphur.
Type:
Article
Language:
en
Keywords:
sulphur isotope; Shetland ophiolite; mineralization; Ni; Fe; Cu
ISSN:
0371-7453
Rights:
Author can archive post-print (ie final draft post-refereeing). For full details see http://www.sherpa.ac.uk/romeo/ [Accessed 12/05/2010]
Citation Count:
3 [Scopus, 12/05/2010]

Full metadata record

DC FieldValue Language
dc.contributor.authorMaynard, J. B. (Jon)en
dc.contributor.authorPrichard, H. M. (Hazel)en
dc.contributor.authorIxer, R. A. F. (Rob)en
dc.contributor.authorLord, R. A. (Richard)en
dc.contributor.authorWright, I. P. (Ian)en
dc.contributor.authorPillinger, C. (Colin)en
dc.contributor.authorMcConville, P.en
dc.contributor.authorBoyce, A. J. (Adrian)en
dc.contributor.authorFallick, A. (Anthony)en
dc.date.accessioned2010-05-12T14:18:29Z-
dc.date.available2010-05-12T14:18:29Z-
dc.date.issued1997-09-
dc.identifier.citationTransactions of the Institutions of Mining and Metallurgy, Section B: Applied Earth Science; 106(Sept-Dec):B215-B226en
dc.identifier.issn0371-7453-
dc.identifier.urihttp://hdl.handle.net/10149/98640-
dc.description.abstractSulphur isotope analyses of 62 samples from the Shetland ophiolite, Scotland, show that the sulphides throughout the igneous stratigraphy have a magmatic signature with the exception of the uppermost gabbros and the lowermost basal thrust talc-carbonate lithologies. Mean δ34S values for whole-rock samples from harzburgite (+3.5‰), dunite pods in harzburgite (+4.3‰), crustal dunite and wehrlite units (+2.5‰), the main pyroxenite unit (+2.9‰), the high-level pyroxenite (+4.1‰) and gabbro (+4.3‰) suggest that the primary sulphides derived their sulphur from a magmatic source enriched in 34S, which is compatible with the supra-subduction zone origin proposed for the Shetland ophiolite. δ34S values for pyrite mineralization in a gabbro, amphibole pegmatite and plagiogranite from the uppermost part of the gabbros range from +9.6 to +14.0‰ and are thought to result from precipitation from a 34S-enriched fluid, which, by analogy with other studies of ophiolitic crust, could have been derived from sea-water sulphate. A sulphide-bearing dunite from a dunite pod in mantle harzburgite at the Cliff locality that contains 4 ppm ∑Pt + Pd has an average δ34S value of +4.2‰, indistinguishable from values from other non-mineralized dunites from dunite pods and indicating a magmatic origin for this sulphur. In contrast, talc-carbonate altered rocks from the basal thrust, including samples from close to the Cliff locality, have an anomalously low mean δ34S value of +0.8‰, which can be explained by introduction of a proportion of isotopically light sulphur from the underlying metasedimentary sequence, which has a mean δ34S of -4.2‰. Stepped combustion analysis supports mineralogical observations that the majority of the sulphur is contained in disseminated Ni, Fe and Cu sulphides. δ34S laser probe data for intergrown pentlandite and heazlewoodite from the crustal dunite unit are essentially identical, which supports the idea that the replacement of pentlandite by heazlewoodite during serpentinization is isochemical with respect to sulphur.en
dc.language.isoenen
dc.publisherManey Publishingen
dc.rightsAuthor can archive post-print (ie final draft post-refereeing). For full details see http://www.sherpa.ac.uk/romeo/ [Accessed 12/05/2010]en
dc.subjectsulphur isotopeen
dc.subjectShetland ophioliteen
dc.subjectmineralizationen
dc.subjectNien
dc.subjectFeen
dc.subjectCuen
dc.titleSulphur isotope study of Ni-Fe-Cu mineralization in the Shetland ophioliteen
dc.typeArticleen
dc.contributor.departmentUniversity of Sunderlanden
dc.identifier.journalTransactions of the Institutions of Mining and Metallurgy, Section B: Applied Earth Scienceen
ref.citationcount3 [Scopus, 12/05/2010]en
or.citation.harvardMaynard, J. et. al. (1997) 'Sulphur isotope study of Ni-Fe-Cu mineralization in the Shetland ophiolite', Transactions of the Institutions of Mining and Metallurgy, Section B: Applied Earth Science, 106 (Sept-Dec), pp.B215-B226.-
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