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A monoclinic post-stishovite polymorph of silica in the Shergotty meteorite
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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2000 (English)In: SCIENCE, ISSN 0036-8075, Vol. 288, no 5471, 1632-1634 p.Article in journal (Refereed) Published
Abstract [en]

A post-stishovite phase of silica was identified in the Shergotty meteorite by x-ray diffraction and field emission scanning electron microscopy. The diffraction pattern revealed a monoclinic Lattice, similar to the baddeleyite-structured polymorph with t

Place, publisher, year, edition, pages
AMER ASSOC ADVANCEMENT SCIENCE , 2000. Vol. 288, no 5471, 1632-1634 p.
Keyword [en]
PEROVSKITE MGSIO3; PRESSURE; PHASE; MANTLE; TRANSITION; HISTORY
Identifiers
URN: urn:nbn:se:uu:diva-37704OAI: oai:DiVA.org:uu-37704DiVA: diva2:65603
Note
Addresses: El Goresy A, Max Planck Inst Chem, J Becher Weg 27, D-55128 Mainz, Germany. Max Planck Inst Chem, D-55128 Mainz, Germany. Uppsala Univ, Inst Earth Sci, Theoret Geochem Program, S-75236 Uppsala, Sweden. Arizona State Univ, Dept Geol, Tempe, AZ 8Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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