Source:http://linkedlifedata.com/resource/pubmed/id/16372006
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Predicate | Object |
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rdf:type | |
lifeskim:mentions | |
pubmed:issue |
7071
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pubmed:dateCreated |
2005-12-22
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pubmed:abstractText |
The post-perovskite phase of (Mg,Fe)SiO3 is believed to be the main mineral phase of the Earth's lowermost mantle (the D'' layer). Its properties explain numerous geophysical observations associated with this layer-for example, the D'' discontinuity, its topography and seismic anisotropy within the layer. Here we use a novel simulation technique, first-principles metadynamics, to identify a family of low-energy polytypic stacking-fault structures intermediate between the perovskite and post-perovskite phases. Metadynamics trajectories identify plane sliding involving the formation of stacking faults as the most favourable pathway for the phase transition, and as a likely mechanism for plastic deformation of perovskite and post-perovskite. In particular, the predicted slip planes are {010} for perovskite (consistent with experiment) and {110} for post-perovskite (in contrast to the previously expected {010} slip planes). Dominant slip planes define the lattice preferred orientation and elastic anisotropy of the texture. The {110} slip planes in post-perovskite require a much smaller degree of lattice preferred orientation to explain geophysical observations of shear-wave anisotropy in the D'' layer.
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pubmed:language |
eng
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pubmed:journal | |
pubmed:status |
PubMed-not-MEDLINE
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pubmed:month |
Dec
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pubmed:issn |
1476-4687
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pubmed:author | |
pubmed:issnType |
Electronic
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pubmed:day |
22
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pubmed:volume |
438
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pubmed:owner |
NLM
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pubmed:authorsComplete |
Y
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pubmed:pagination |
1142-4
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pubmed:year |
2005
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pubmed:articleTitle |
Anisotropy of Earth's D'' layer and stacking faults in the MgSiO3 post-perovskite phase.
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pubmed:affiliation |
Laboratory of Crystallography, Department of Materials, ETH Zurich, HCI G 515, Wolfgang-Pauli-Strasse 10, CH-8093 Zurich, Switzerland. a.oganov@mat.ethz.ch
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pubmed:publicationType |
Journal Article
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