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- W1998726642 abstract "Research Article| February 01, 1973 Delimitation of the Hematite-Ilmenite Miscibility Gap D. H. LINDSLEY D. H. LINDSLEY 1Department of Earth and Space Sciences, State University of New York, Stony Brook, New York 11790 Search for other works by this author on: GSW Google Scholar Author and Article Information D. H. LINDSLEY 1Department of Earth and Space Sciences, State University of New York, Stony Brook, New York 11790 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1973) 84 (2): 657–662. https://doi.org/10.1130/0016-7606(1973)84<657:DOTHMG>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation D. H. LINDSLEY; Delimitation of the Hematite-Ilmenite Miscibility Gap. GSA Bulletin 1973;; 84 (2): 657–662. doi: https://doi.org/10.1130/0016-7606(1973)84<657:DOTHMG>2.0.CO;2 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 SocietyGSA Bulletin Search Advanced Search Abstract Note: This paper is dedicated to Aaron and Elizabeth Waters on the occasion of Dr. Waters' retirement.Recent analytical data on the compositions of natural hematite-ilmenite solid solutions suggest that the miscibility gap of Carmichael (1961) cannot be correct. Attempts to redetermine the miscibility gap under hydrothermal conditions have been only partly successful, for with the oxygen buffers currently available, it is not possible to retain both hematite and ilmenite phases in a given experiment. Despite the fact that the hydrothermal experiments do not give the maximum solubilities of Fe2O3 in ilmenite and FeTiO3 in hematite, they nevertheless show that the published miscibility gap is too wide (by approximately 15 mole percent at 600°C) and that the consolute temperature is at least 150°C too high. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal 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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- W1998726642 title "Delimitation of the Hematite-Ilmenite Miscibility Gap" @default.
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