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Economic Geology; January 2005; v. 100; no. 1; p. 7-28; DOI: 10.2113/100.1.0007
© Society of Economic Geologists

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FIG. 12. Summary of the SHRIMP ages obtained in this study compared to conventional U-Pb zircon ages and Rb-Sr bulk-rock ages of the Estrela Granitic Complex, the Old Salobo Granite, the Itacaiúnas Granite, Re-Os ages of molybdenite, and Pb-Pb model ages of bornite-chalcopyrite-magnetite mineralization at Salobo, and the host metavolcanic rocks of the Igarapé Bahia deposit.

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