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Chemical interaction of Fe and Al2O3 as a source of heterogeneity at the Earth's core-mantle boundary
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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2001 (English)In: NATURE, ISSN 0028-0836, Vol. 412, no 6846, 527-529 p.Article in journal (Refereed) Published
Abstract [en]

Seismological studies have revealed that a complex texture or heterogeneity exists in the Earth's inner core and at the boundary between core and mantle(1-4). These studies highlight the importance of understanding the properties of iron when modelling th

Place, publisher, year, edition, pages
MACMILLAN PUBLISHERS LTD , 2001. Vol. 412, no 6846, 527-529 p.
Keyword [en]
DIAMOND-ANVIL CELL; X-RAY-DIFFRACTION; HIGH-PRESSURE; LIQUID-IRON; INNER-CORE; PEROVSKITE; SILICATES; GPA; SPECTROSCOPY; MOSSBAUER
Identifiers
URN: urn:nbn:se:uu:diva-37820OAI: oai:DiVA.org:uu-37820DiVA: diva2:65719
Note
Addresses: Dubrovinsky L, Uppsala Univ, Dept Earth Sci, S-75336 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, S-75336 Uppsala, Sweden. Max Planck Inst Met Forsch, D-70569 Stuttgart, Germany. 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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