Anelasticity and microcreep in polycrystalline MgO at high temperature: an exploratory study

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dc.contributor.authorWebb, Sharon
dc.contributor.authorJackson, Ian
dc.date.accessioned2015-12-13T23:40:51Z
dc.date.available2015-12-13T23:40:51Z
dc.date.issued2003
dc.date.updated2015-12-12T09:30:25Z
dc.description.abstractThe frequency dependence of the shear modulus and dissipation in polycrystalline MgO has been determined at high temperature using both microcreep (ε = 10-4) and seismic frequency forced-oscillation (ε = 10-5) measurements. The frequency-dependent and t
dc.identifier.issn0342-1791
dc.identifier.urihttp://hdl.handle.net/1885/94619
dc.publisherSpringer
dc.sourcePhysics and Chemistry of Minerals
dc.subjectKeywords: Anelastic relaxation; Creep; Deformation; Grain boundaries; Magnesia; Oscillations; Seismology; Slip forming; Viscoelasticity; Microcreep; Polycrystalline materials; anelasticity; creep; grain boundary; high temperature; perovskite; seismic wave; viscoela Anelasticity; Forced oscillation; MgO; Micro-creep; Seismic frequency; Viscoelasticity
dc.titleAnelasticity and microcreep in polycrystalline MgO at high temperature: an exploratory study
dc.typeJournal article
local.bibliographicCitation.lastpage166
local.bibliographicCitation.startpage157
local.contributor.affiliationWebb, Sharon, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationJackson, Ian, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidWebb, Sharon, u1550843
local.contributor.authoruidJackson, Ian, u7800055
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor020406 - Surfaces and Structural Properties of Condensed Matter
local.identifier.absfor040499 - Geophysics not elsewhere classified
local.identifier.ariespublicationMigratedxPub24244
local.identifier.citationvolume30
local.identifier.doi10.1007/s00269-003-0299-1
local.identifier.scopusID2-s2.0-0038656434
local.type.statusPublished Version

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