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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:28:25Z</responseDate> <request identifier=oai:HAL:hal-01054330v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01054330v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:phys</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:INC-CNRS</setSpec> <setSpec>collection:ENSC-LILLE</setSpec> <setSpec>collection:INRA</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Characterization of the glide planes of the [001] screw dislocations in olivine using electron tomography</title> <creator>Mussi, Alexandre</creator> <creator>Cordier, Patrick</creator> <creator>Demouchy, Sylvie</creator> <creator>Vanmansart, Claude</creator> <contributor>Unité Matériaux et Transformations - UMR 8207 (UMET) ; Centre National de la Recherche Scientifique (CNRS) - Ecole Nationale Supérieure de Chimie de Lille (ENSCL) - Institut National de la Recherche Agronomique (INRA) - Université de Lille, Sciences et Technologies</contributor> <contributor>Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor> <description>International audience</description> <source>ISSN: 0342-1791</source> <source>EISSN: 1432-2021</source> <source>Physics and Chemistry of Minerals</source> <publisher>Springer Verlag</publisher> <identifier>hal-01054330</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01054330</identifier> <source>https://hal.archives-ouvertes.fr/hal-01054330</source> <source>Physics and Chemistry of Minerals, Springer Verlag, 2014, 41 (7), pp.537-545. 〈10.1007/s00269-014-0665-1〉</source> <identifier>DOI : 10.1007/s00269-014-0665-1</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00269-014-0665-1</relation> <language>en</language> <subject lang=en>Olivine</subject> <subject lang=en>Tomography</subject> <subject lang=en>Precession</subject> <subject lang=en>TEM</subject> <subject lang=en>Dislocation</subject> <subject lang=en>Glide plane</subject> <subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject> <subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>A San Carlos olivine polycrystal has been deformed under uppermost mantle conditions, by compression at 900 °C, at a strain rate of 1.1 × 10−5 s−1, under a confining pressure of 300 MPa, using the Paterson press. Transmission electron tomography of dislocations has been performed by scanning transmission electron microscopy, by conventional transmission electron microscopy using the weak-beam dark-field technique, associated with precession or not, in order to determine the glide planes of [001] screw dislocations. This recent technique is the most suitable one since most [001] dislocations exhibit straight screw segments due to the high lattice friction on this character at low temperature. We find that [001] dislocations glide in (100), (010) and {110} as already reported, but also more unexpectedly in {120} and {130}. We show that at 900 °C, [001] {110} glide is dominant in polycrystals. We have, however, noted and characterized numerous cross-slip events in the specimen.</description> <date>2014-07</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>