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Economic Geology; June 2000; v. 95; no. 4; p. 831-844; DOI: 10.2113/95.4.831
© 2000 Society of Economic Geologists
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Oxygen Isotope Studies of the Voisey’s Bay Ni-Cu-Co Deposit, Labrador, Canada

Edward M. Ripley{dagger} and Young-Rok Park

Department of Geological Sciences, Indiana University, Bloomington, Indiana 47405

Chusi Li

Department of Earth Sciences, University of Pretoria, Pretoria 0002, South Africa

A. J. Naldrett

Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1

{dagger} Corresponding author: e-mail, ripley{at}indiana.edu

Oxygen isotope studies of the Voisey’s Bay intrusion and surrounding country rocks were initiated to help assess the importance of magma contamination in the generation of Ni-Cu-Co sulfide mineralization. The {delta}18O values of Proterozoic Tasiuyak paragneiss country rocks range from 8.3 to 16.1 per mil, whereas those of enderbitic and mafic orthogneiss range from 5.7 to 8.7 per mil, with most values less than 7.5 per mil. The {delta}18O values of the principal units of the Voisey’s Bay intrusion fall in the range of 5.4 to 7.7 per mil, with over 90 percent of the samples less than 7 per mil and not indicative of magma contamination. Strong evidence for country-rock contamination of the mafic magma comes from inclusions of paragneiss found in the basal breccia sequence of the Eastern Deeps and the feeder breccia in the Reid Brook zone. The gneiss inclusions range in {delta}18O values from 4.7 to 10.6 per mil and are depleted in 18O relative to parental paragneiss country rocks. Loss of a siliceous, 18O-rich component has accompanied progressive conversion of the xenoliths to residual assemblages rich in plagioclase and hercynite. Elevated {delta}18O values (up to 9.3{per thousand}) are found in troctolitic and noritic matrix of the breccias but are restricted to distances less than 2 cm from the margins of inclusions. These isotopic exchange profiles have been produced during subsolidus cooling and do not record the transport of the major high 18O component lost from the gneiss. Oxygen isotope evidence in the igneous rocks for assimilation of high 18O material derived from the gneiss is thought to have been destroyed via dilution as large volumes of magma moved from lower to higher chambers through a conduit system. The introduction of the high 18O, SiO2-rich contaminant may have acted in concert with the introduction of country-rock sulfide in promoting sulfide saturation of the Voisey’s Bay magma.




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