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Stability of (Mg0.5Fe0.5)O and (Mg0.8Fe0.2)O magnesiowustites in the lower mantle
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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2001 (English)In: EUROPEAN JOURNAL OF MINERALOGY, ISSN 0935-1221, Vol. 13, no 5, 857-861 p.Article in journal (Refereed) Published
Abstract [en]

We have heated magnesiowtistites (Mg0.5Fe0.5)O and (Mg0.8Fe0.2)O to temperatures of over 1000 K at pressures of over 80 GPa simulating the stability of the solid solution at physical conditions relevant to the Earth's lower mantle. The X-ray study of the

Place, publisher, year, edition, pages
E SCHWEIZERBARTSCHE VERLAGS , 2001. Vol. 13, no 5, 857-861 p.
Keyword [en]
magnesiowustite; high pressure; immiscibility; Earth's lower mantle; diamond-anvil cell; DIAMOND-ANVIL CELL; X-RAY-DIFFRACTION; HIGH-PRESSURE; FEO; STATE; TEMPERATURE; EQUATION; WUSTITE; PHASE; MINERALOGY
Identifiers
URN: urn:nbn:se:uu:diva-37821OAI: oai:DiVA.org:uu-37821DiVA: diva2:65720
Note
Addresses: Dubrovinsky L, Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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