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dc.contributor.author Tommaseo C.E.
dc.contributor.author Merkel S.
dc.contributor.author Speziale S.
dc.contributor.author Wenk H.R.
dc.contributor.author Devine J.
dc.date.accessioned 2025-04-19T06:19:38Z
dc.date.available 2025-04-19T06:19:38Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=14728200
dc.identifier.citation Physics and Chemistry of Minerals, 2006, 33, 2, 84-97
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48976
dc.description.abstract Cubic magnesiowustite has been deformed in a diamond anvil cell at room temperature. We present results for (Mg0.4Fe0.6)O, (Mg0.25Fe0.75)O, and (Mg0.1 Fe0.9)O up to 37, 16, and 18 GPa, respectively. The diffraction images, obtained with the radial diffraction technique, are analyzed using both single peak intensities and a Rietveld method. For all samples, we observe a [100] fiber texture but the texture strength decreases with increasing iron content. This texture pattern is consistent with {110}-〈1-10〉 slip. The images were also analyzed for stress, elastic strains, and elastic anisotropy. In general, the stress measured in magnesiowustite samples is lower than previously measured on MgO. The elastic anisotropy deduced from the X-ray measurements shows a broad agreement with models based on measurements with other techniques. © Springer-Verlag 2006.
dc.subject (MG,FE)O
dc.subject DAC
dc.subject DEFORMATION MECHANISMS
dc.subject ELASTICITY
dc.subject MAGNESIOWUSTITE
dc.subject SYNCHROTRON X-RAYS
dc.subject TEXTURE
dc.title TEXTURE DEVELOPMENT AND ELASTIC STRESSES IN MAGNESIOWUSTITE AT HIGH PRESSURE
dc.type Статья
dc.identifier.doi 10.1007/s00269-005-0054-x


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