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• W2000618267 abstract "Research Article| February 01, 2013 Banded iron formation to iron ore: A record of the evolution of Earth environments? K.A. Evans; K.A. Evans 1Department of Applied Geology, Curtin University, GPO Box U1987, WA 6845, Australia Search for other works by this author on: GSW Google Scholar T.C. McCuaig; T.C. McCuaig 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia Search for other works by this author on: GSW Google Scholar D. Leach; D. Leach 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia Search for other works by this author on: GSW Google Scholar T. Angerer; T. Angerer 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia Search for other works by this author on: GSW Google Scholar S.G. Hagemann S.G. Hagemann 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information K.A. Evans 1Department of Applied Geology, Curtin University, GPO Box U1987, WA 6845, Australia T.C. McCuaig 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia D. Leach 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia T. Angerer 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia S.G. Hagemann 2Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, Crawley, Perth, WA 6009, Australia Publisher: Geological Society of America Received: 27 Jan 2012 Revision Received: 02 Aug 2012 Accepted: 18 Aug 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (2): 99–102. https://doi.org/10.1130/G33244.1 Article history Received: 27 Jan 2012 Revision Received: 02 Aug 2012 Accepted: 18 Aug 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation K.A. Evans, T.C. McCuaig, D. Leach, T. Angerer, S.G. Hagemann; Banded iron formation to iron ore: A record of the evolution of Earth environments?. Geology 2013;; 41 (2): 99–102. doi: https://doi.org/10.1130/G33244.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Banded iron formations (BIF) are the protolith to most of the world’s largest iron ore deposits. Previous hypogene genetic models for Paleoproterozoic “Lake Superior” BIF-hosted deposits invoke upwards, down-temperature flow of basinal brines via complex silica and carbonate precipitation/dissolution processes. Such models are challenged by the necessary SiO2 removal. Thermodynamic and mass balance constraints are used to refine conceptual models of the formation of BIF-hosted iron ore. These constraints, plus existing isotope and halogen ratio evidence, are consistent with removal of silica by down- or up-directed infiltration of high-pH hypersaline brines, with or without a contribution from basinal brines. The proposed link to surface environments suggest that Paleoproterozoic BIF-ore upgrade may provide a record of a critical time in the evolution of the Earth’s biosphere and hydrosphere. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2000618267 title "Banded iron formation to iron ore: A record of the evolution of Earth environments?" @default.
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