Isotopic constraints on fluid evolution and precipitation mechanisms for the Boléo Cu–Co–Zn district, Mexico

Author:

Conly Andrew G.,Beaudoin Georges,Scott Steven D.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference92 articles.

1. Allan JR, Matthews RK (1982) Isotopic signatures associated with early meteoric diagenesis: Sedimentology 29:797–817

2. Anderson GM, Garven G (1987) Sulfate–sulfide–carbonate associations in Mississippi Valley-type lead–zinc deposits. Econ Geol 82:482–488

3. Atwater T (1989) Plate tectonic history, northeastern Pacific and western North America. In: Winterer EL, Hussong DM, Decker RW (eds) The eastern Pacific Ocean and Hawaii. The Geology of North America. Geol Soc Am Bull, N:21–72

4. Bailes RJ, Christoffersen JC, Escandon VF, Peatfield GR (2001) Sediment-hosted deposits of the Boléo copper–cobalt–zinc district, Baja California Sur, Mexico. Soc Econ Geol (Spec Publ) 8:291–306

5. Bar-Matthews M, Matthews A (1990) Chemical and stable isotope fraction in manganese oxide-phosphorite mineralization, Timna Valley, Israel. Geol Mag 127:1–12

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