Magnetite solubility and iron transport in magmatic-hydrothermal environments

Simon, Adam C.; Pettke, Thomas; Candela, Philip A.; Piccoli, Philip M.; Heinrich, Christoph A.

doi:10.1016/j.gca.2004.05.033

Cited by 194Geological and Geochemical AnalysisHigh-pressure geophysics and materialsMetallurgical Processes and Thermodynamics

Magnetite solubility and iron transport in magmatic-hydrothermal environments

Simon, Adam C., Pettke, Thomas, Candela, Philip A., Piccoli, Philip M., Heinrich, Christoph A.·2004·Geochimica et Cosmochimica Acta

DOI 10.1016/j.gca.2004.05.033

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δ56Fe values should remain relatively unchanged due to low solubility of iron in aqueous solutions at hydrothermal temperatures, slow diffusion of Fe in hematite and magnetite, and lack of a large external reservoir for equilibration.
“δ 56 Fe values should remain relatively unchanged due to the low solubility of iron in aqueous solutions at hydrothermal temperatures (Chou and Eugster, 1977; Simon et al., 2004), slow diffusion of Fe in hematite and magnetite (Hallstrom et al., 2011), and lack of a large external reservoir for equilibration”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Simon et al., 2004

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RETRACTED ARTICLE: Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses
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Authors: Simon, A. C., Pettke, T., Candela, P. A., Piccoli, P. M., & Heinrich, C. A.
Affiliations: University of Maryland, College Park (US)
ETH Zurich (CH)
Corresponding author: Simon, Adam C.
ORCID: Simon, Adam C.
Pettke, Thomas
Piccoli, Philip M.
Heinrich, Christoph A.
Venue: Geochimica et Cosmochimica Acta
Publisher: Elsevier BV
Published: 2004-12
Volume: 68
Issue: 23
Pages: 4905-4914
ISSN: 0016-7037 (ISSN-L)
DOI: 10.1016/j.gca.2004.05.033
OpenAlex: W2091971395
Cited by: 194
References: 46
Citations by year: 2026: 13 · 2025: 13 · 2024: 14 · 2023: 11 · 2022: 11 · 2021: 13 · 2020: 17 · 2019: 11 · 2018: 9 · 2017: 17 · 2016: 8 · 2015: 13 · 2014: 6 · 2013: 5 · 2012: 6
FWCI: 1.75
Type: journal article
Language: en
Open access: closed
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Geochimica et Cosmochimica Acta (publishedVersion)
BORIS (University Library Bern) (submittedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
Physical Sciences › Engineering › Mechanical Engineering › Metallurgical Processes and Thermodynamics
Keywords: iron transport, magmatic-hydrothermal systems, pressure dependence, fluid inclusions, hydrogen chloride, iron speciation

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