Contrasting fluids and reservoirs in the contiguous Marcona and Mina Justa iron oxide–Cu (–Ag–Au) deposits, south-central Perú

Author:

Chen Huayong,Kyser T. Kurtis,Clark Alan H.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference101 articles.

1. Adshead ND, Voulgaris P, Muscio VN (1998) Osborne copper–gold deposit. In: Berkman DA, Mackenzie DH (eds) Geology of Australian and Papua New Guinean mineral deposits. The Australasian Institute of Mining and Metallurgy, Melbourne, pp 793–799

2. Aguirre L (1988) Chemical mobility during low-grade metamorphism of a Jurassic lava flow: Río Grande Formation, Peru. J S Am Earth Sci 1:343–361

3. Alt JC (1999) Very low-grade hydrothermal metamorphism of basic igneous rocks. In: Frey M, Robinson D (eds) Low-grade metamorphism. Blackwell Science, Oxford, pp 169–201

4. Atherton MP, Webb S (1989) Volcanic facies, structure, and geochemistry of the marginal basin rocks of central Peru. J S Am Earth Sci 2:241–261

5. Baker T (1998) Alteration, mineralization, and fluid evolution at the Eloise Cu–Au deposit, Cloncurry District, Northwest Queensland, Australia. Econ Geol 93:1213–1236

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