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Stability of ferropericlase in the lower mantle
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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2000 (English)In: SCIENCE, ISSN 0036-8075, Vol. 289, no 5478, 430-432 p.Article in journal (Refereed) Published
Abstract [en]

We have heated ferropericlases (Mg0.60Fe0.40)O and (Mg0.50Fe0.50)O to temperatures of 1000 kelvin at pressures of 86 gigapascals, simulating the stability of the solid solution at physical conditions relevant to Earth's lower mantle. The in situ x-ray stu

Place, publisher, year, edition, pages
AMER ASSOC ADVANCEMENT SCIENCE , 2000. Vol. 289, no 5478, 430-432 p.
Keyword [en]
HIGH-PRESSURE; FEO; TEMPERATURE; COLLAPSE; EQUATION; WUSTITE; STATE; MGO; GPA
Identifiers
URN: urn:nbn:se:uu:diva-37697OAI: oai:DiVA.org:uu-37697DiVA: diva2:65596
Note
Addresses: Dubrovinsky LS, Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden. European Synchrotron Radiat Facil, F-38043 Grenoble, France.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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