Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems

Research output: Chapter in Book/Report/Conference proceedingChapter

77 Citations (Scopus)

Abstract

The Fe oxide(-Cu-Au-REE-P-U) family of Cu, Fe, and/or Au deposits (or IOCG) represents a geochemically coherent but geologically diverse group that formed globally from the Archean to the Holocene. IOCG systems exhibit intense, voluminous Na-Ca-K-Fe(-H) hydrothermal alteration related to flow of moderately to highly saline metal-rich, sulfur-poor brines. These fluids account for the characteristic sulfide-poor, oxide-rich mineralogy and the alkali-rich character of the alteration and for the varied contents of Cu, Au, and other metals. Associated igneous rocks range from mafic to felsic, subalkaline to alkaline. Metal enrichments vary with host-rock type and sulfur availability. Geologic settings are tectonically diverse but commonly have evidence for contemporaneous or older evaporitic environments. Magmatism drives most systems, yet clearly amagmatic examples occur. Geochemical and petrologic studies demonstrate igneous-dominated sources for some solutes and permissive evidence for a connection to magmatic fluids. In many cases, a central role for nonmagmatic saline fluids is evident. The geochemistry of the latter fluids rationalizes the key distinguishing features of the IOCG family. The diversity of the IOCG family parallels that seen in other major families of deposits; their distinctive attributes indicate that they comprise a separate class of (mainly) terrestrial hydrothermal systems.

Original languageEnglish (US)
Title of host publicationTreatise on Geochemistry: Second Edition
PublisherElsevier Inc.
Pages515-541
Number of pages27
Volume13
ISBN (Print)9780080983004
DOIs
StatePublished - Nov 2013

Fingerprint

iron oxide
rare earth element
Fluids
fluid
Metals
Sulfur
Oxides
metal
Deposits
sulfur
oxide
Igneous rocks
Brines
Geochemistry
Mineralogy
Alkalies
Sulfides
hydrothermal system
hydrothermal alteration
igneous rock

Keywords

  • Alkali metasomatism
  • Iron oxide(-copper-gold)
  • Kiruna
  • Olympic Dam
  • Terrestrial hydrothermal

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)
  • Chemistry(all)

Cite this

Barton, M. D. (2013). Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. In Treatise on Geochemistry: Second Edition (Vol. 13, pp. 515-541). Elsevier Inc.. https://doi.org/10.1016/B978-0-08-095975-7.01123-2

Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. / Barton, Mark D.

Treatise on Geochemistry: Second Edition. Vol. 13 Elsevier Inc., 2013. p. 515-541.

Research output: Chapter in Book/Report/Conference proceedingChapter

Barton, MD 2013, Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. in Treatise on Geochemistry: Second Edition. vol. 13, Elsevier Inc., pp. 515-541. https://doi.org/10.1016/B978-0-08-095975-7.01123-2
Barton MD. Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. In Treatise on Geochemistry: Second Edition. Vol. 13. Elsevier Inc. 2013. p. 515-541 https://doi.org/10.1016/B978-0-08-095975-7.01123-2
Barton, Mark D. / Iron Oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. Treatise on Geochemistry: Second Edition. Vol. 13 Elsevier Inc., 2013. pp. 515-541
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