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Stability of perovskite (MgSiO3) in the Earth's mantle
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Solid Earth Geology.
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1996 (English)In: SCIENCE, ISSN 0036-8075, Vol. 274, no 5291, 1357-1359 p.Article in journal (Refereed) Published
Abstract [en]

Available thermodynamic data and seismic models favor perovskite (MgSiO3) as the stable phase in the mantle. MgSiO3 was heated at temperatures from 1900 to 3200 kelvin with a Nd-YAG laser in diamond-anvil cells to study the phase relations at pressures fr

Place, publisher, year, edition, pages
1996. Vol. 274, no 5291, 1357-1359 p.
Keyword [en]
STISHOVITE; PHASE
Identifiers
URN: urn:nbn:se:uu:diva-27901OAI: oai:DiVA.org:uu-27901DiVA: diva2:55797
Note
Addresses: Saxena SK, UPPSALA UNIV, INST EARTH SCI, S-75236 UPPSALA, SWEDEN. EUROPEAN SYNCHROTRON RADIAT FACIL, F-38043 GRENOBLE, FRANCE. CARNEGIE INST WASHINGTON, GEOPHYS LAB, CTR HIGH PRESSURE RES, WASHINGTON, DC 20015.Available from: 2006-12-01 Created: 2006-12-01 Last updated: 2011-01-15

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Lazor, P

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