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Separating intrinsic and apparent anisotropy

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dc.contributor.authorFichtner, Andreas
dc.contributor.authorKennett, Brian
dc.contributor.authorTrampert, Jeannot
dc.date.accessioned2015-12-13T22:24:35Z
dc.date.issued2013
dc.date.updated2016-02-24T09:10:52Z
dc.description.abstractSeismic anisotropy plays a key role in studies of the Earth's rheology and deformation because of its relation to flow-induced lattice-preferred orientation (LPO) of intrinsically anisotropic minerals. In addition to LPO, small-scale heterogeneity produce
dc.identifier.issn0031-9201
dc.identifier.urihttp://hdl.handle.net/1885/72797
dc.publisherElsevier
dc.sourcePhysics of the Earth and Planetary Interiors
dc.subjectKeywords: Intrinsic anisotropy; Lattice preferred orientation; Mantle convection; Seismic anisotropy; Seismic tomography; Anisotropic media; Deformation; Elasticity; Seismic prospecting; Seismology; Surface waves; Anisotropy; deformation; geodynamics; inversion tec Apparent anisotropy; Intrinsic anisotropy; Lattice-preferred orientation; Mantle convection; Seismic anisotropy; Seismic tomography
dc.titleSeparating intrinsic and apparent anisotropy
dc.typeJournal article
local.bibliographicCitation.lastpage20
local.bibliographicCitation.startpage11
local.contributor.affiliationFichtner, Andreas, Swiss Federal Institute of Technology
local.contributor.affiliationKennett, Brian, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationTrampert, Jeannot, Utrecht University
local.contributor.authoruidKennett, Brian, u8413736
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040407 - Seismology and Seismic Exploration
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB3433
local.identifier.citationvolume219
local.identifier.doi10.1016/j.pepi.2013.03.006
local.identifier.scopusID2-s2.0-84878191748
local.identifier.thomsonID000320825700002
local.type.statusPublished Version

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