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Re–Os and Pb–Pb geochronology of the Archean Salobo iron oxide copper–gold deposit, Carajás mineral province, northern Brazil

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Abstract

Rhenium–osmium ages were determined for two molybdenite samples and a Pb–Pb age was derived from bornite–chalcopyrite–magnetite at the Salobo iron oxide copper–gold deposit to determine the timing of mineralization and its relation to the nearby Old Salobo Granite. Rhenium–osmium dating of molybdenite spatially associated with copper sulfide minerals yields ages with weighted means of 2576±8 and 2562±8 Ma. Removing the error multiplier introduced by the decay constant uncertainty, appropriate for comparing ages from the same isotopic system, these data convincingly argue for two temporally separated pulses of molybdenite deposition at 2576.1±1.4 Ma (n=2) and 2561.7±3.1 Ma (n=3). The 2576±8 Ma age coincides with a previously published U–Pb age of 2573±2 Ma for the Old Salobo Granite, suggesting that main stage ore formation may have been contemporaneous with granite magmatism. The slightly younger 2562 Ma age most likely represents new molybdenite precipitation associated with the development or reactivation of local shear zones. Lead–lead stepwise leaching of copper sulfide minerals yields a less precise isochron age of 2579±71 Ma, and supports an Archean age for the Salobo ores. This is the first documentation of an Archean iron oxide copper–gold deposit, and the Re–Os and Pb–Pb geochronology herein support 2580–2550 Ma estimates for basement reactivation and regional granite magmatism associated with the development of brittle–ductile shear zones.

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Acknowledgements

We are grateful to G. Brown and N. Grant from Anglo-American Plc for financing the initial Re–Os analyses of the two molybdenite samples. We also appreciate the CVRD's logistic support during the field campaign. Richard Markey, AIRIE-Colorado State University, provided the Re–Os analyses. This work was supported by a Swiss SNF grant and was supplemented by funds from NSF EAR-0087483 (Stein) for added replicate analyses needed to establish the separation of ages for the two molybdenites. Journal reviewers David Selby and Pat Williams, as well as Richard Goldfarb, provided insightful and helpful comments.

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Correspondence to Karin Requia.

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Requia, K., Stein, H., Fontboté, L. et al. Re–Os and Pb–Pb geochronology of the Archean Salobo iron oxide copper–gold deposit, Carajás mineral province, northern Brazil. Miner Deposita 38, 727–738 (2003). https://doi.org/10.1007/s00126-003-0364-1

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