A trace metal, stable isotope (H, O, S), and geochronological (U-Pb titanite) characterization of hybridized gold orebodies in the Missanabie-Renabie district, Wawa subprovince (Canada)

Author:

McDivitt Jordan A.,Kontak Daniel J.,Lafrance Bruno,Petrus Joseph A.,Fayek Mostafa

Funder

NSERC

Ontario Geological Survey

Society of Economic Geologists

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference95 articles.

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2. Aleinikoff JN, Wintsch RP, Tollo RP, Unruh DM, Fanning CM, Schmitz MD (2007) Ages and origins of rocks of the Killingworth dome, south-Central Connecticut: implications for the tectonic evolution of southern New England. J Sci 307:63–118

3. Beaudoin G (2011) The stable isotope geochemistry of orogenic gold deposits. In: Barra F, Reich M, Campos E, Tornos F (eds) Proceedings of the Eleventh Biennial SGA Meeting, Antofagasta, pp 556–558

4. Beaudoin G, Pitre D (2005) Stable isotope geochemistry of the Archean Val-d’Or (Canada) orogenic gold vein field. Mineral Deposita 40:59–75

5. Bennett G (1972) Precambrian geology of Stover and Brackin townships. Ontario Geological Survey preliminary map P.2380

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