ArticleThe influence of hydrothermal fluid composition and advection rates on black smoker chimney mineralogy: Insights from modeling transport and reaction
References (50)
- et al.
Chemical evolution of mid-ocean ridge hot springs
Geochitn. Cosmochim. Acta
(1985) - et al.
Flow rates in the axial hot springs of the East Pacific Rise (21°N): implications for the heat budget and the formation of massive sulfide deposits
Earth Planet. Sci. Lett.
(1984) - et al.
Determination of FeCl complexing in the low pressure supercritical region (NaCl fluid): iron solubility constraints on pH of subseafloor hydrothermal fluids
Geochim. Cosmochim. Acta
(1992) - et al.
Experimental study of iron-chloride complexing in hydrothermal fluids
Geochim. Cosmochim. Acta
(1992) - et al.
Hot spring deposits on the East Pacific Rise at 21°N: preliminary description of mineralogy and genesis
Earth Planet. Sci. Lett.
(1981) - et al.
Formation of massive sulfide deposits on oceanic ridge crests: Incremental reaction models for mixing between hydrothermal solutions and seawater
Geochim. Cosmochim. Acta
(1984) - et al.
SUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from I -5000 bars and 0–1000°C
Computers Geosci.
(1992) - et al.
A first principles approach to supergene enrichment of a porphyry copper protore: I. CuFeS subsystem
Geochitn. Cosmochim. Acta
(1992) - et al.
Hydrothermal vent waters at 13°N on the East Pacific Rise: isotopic composition and gas concentration
Earth Planet. Sci. Lett.
(1987) Calculation of multicomponent chemical equilibria and reaction processes in systems involving minerals, gases and an aqueous phase
Geochim. Cosmochim. Acta
(1982)
Effect of silica polymerization and pH on geothermal scaling
Geothermics
Thermodynamic assessment of hydrothermal alkali feldspar- mica-aluminosilicate equilibria
Geochim. Cosmochim. Acta
Growth of large sulfide structures on the Endeavour Segment of the Juan de Fuca Ridge
Earth Planet. Sci. Lett.
The heat and fluid transfer associated with the flanges on hydrothermal venting structures
Earth Planet. Sci. Lett.
Ore solution chemistry: VI. Stabilities of chloride and bisulfide complexes zinc to 350°C
Econ. Geol.
Chemical controls on the composition of vent fluids at 13-11°N 21°N, East Pacific Rise
J. Geophys. Res.
The Endeavour main vent field revisited: phase separation and unusual alkali and boron chemistry
Eos
A time-series of vent fluid compositions from 21°N, East Pacific Rise (1979, 1981, 1985), and the Guaymas Basin, Gulf of California (1982, 1985)
J. Geophys. Res.
Experimental determination of CuCl speciation at the T-P conditions relevant to ridge crest hydrothermal activity: implications to log (fO2) in the hot spring fluids
Eos
Tectonic setting, mineralogical and geochemical zonation in the Snake Pit sulfide deposit (Mid-Atlantic Ridge at 23°N)
Econ. Geol.
The behavior of silica in hydrothermal solutions
Bimetasomatism resulting from intergranular diffusion: I. A theoretical model for monomineralic reaction zone sequences
Amer. J. Sci.
Bimetasomatism resulting from intergranular diffusion: II. Prediction of multimineralic zone sequences
Amer. J. Sci.
The genesis of hot spring deposits on the East Pacific Rise, 21°N
Sulfide-sulfate chimneys on the East Pacific Rise, 11 and 13°N latitudes. Part I: Mineralogy and paragenesis
Can. Mineral.
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A new mode of mineral replacement reactions involving the synergy between fluid-induced solid-state diffusion and dissolution-reprecipitation: A case study of the replacement of bornite by copper sulfides
2022, Geochimica et Cosmochimica ActaCitation Excerpt :Yet the mechanism of such mineral replacement reactions has not been adequately studied. We chose to use the replacement of bornite (Cu5FeS4) by chalcopyrite (CuFeS2) and copper sulfides as a model system to study the interplay between solid-state diffusion and dissolution-reprecipitation processes because cation diffusion in bornite is fast (Grguric and Putnis, 1999), and dissolution-reprecipitation mineral replacement reactions are commonly observed in copper-iron sulfides in many ore deposits (Ciobanu et al., 2017; Cook et al., 2011; Graham et al., 1988; Halbach et al., 1998; Haymon, 1983; Li et al. 2020; Liu et al., 2017; Oszczepalski, 1999; Ramdohr, 1980; Robb, 2005; 2013; Tivey, 1995). The complex ternary Cu-Fe-S system has extensive solid solutions such as the bornite-digenite solid solution (bdss), the high- and low- temperature phases, and the metastable phases, which convolutes textural and mineralogical evolution along the Cu-Fe-S and Cu-S joins (Barton, 1973; Cabri, 1973; Craig and Scott, 1974).