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Stability of KAlSi3O8 hollandite-type structure in the earth's lower mantle conditions
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2001 (English)In: GEOPHYSICAL RESEARCH LETTERS, ISSN 0094-8276, Vol. 28, no 14, 2735-2738 p.Article in journal (Refereed) Published
Abstract [en]

The stability of KAlSi3O8 hollandite-type structure is investigated in a series of synthesis experiments between 20 and 95 GPa at 650(+/- 50) degreesC and between 1200 to 2300 degreesC, using electrically- and laser-heated diamond anvil cells, respectivel

Place, publisher, year, edition, pages
AMER GEOPHYSICAL UNION , 2001. Vol. 28, no 14, 2735-2738 p.
Keyword [en]
HIGH-PRESSURE; CRYSTAL-CHEMISTRY; POTASSIUM; PHASE; EQUATION; STATE; CORE; GPA; TRANSITIONS; TEMPERATURE
Identifiers
URN: urn:nbn:se:uu:diva-37893OAI: oai:DiVA.org:uu-37893DiVA: diva2:65792
Note
Addresses: Tutti F, Uppsala Univ, Inst Earth Sci, SE-75236 Uppsala, Sweden. Uppsala Univ, Inst Earth Sci, SE-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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