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Parallel 3-D Simulation of a Fault Gouge Using the Lattice Solid Model

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dc.contributor.authorLatham, Shane
dc.contributor.authorAbe, Steffen
dc.contributor.authorMora, Peter Ronald
dc.date.accessioned2015-12-10T22:29:03Z
dc.date.issued2006
dc.date.updated2015-12-09T09:52:51Z
dc.description.abstractDespite the insight gained from 2-D particle models, and given that the dynamics of crustal faults occur in 3-D space, the question remains, how do the 3-D fault gouge dynamics differ from those in 2-D? Traditionally, 2-D modeling has been preferred over
dc.identifier.issn0033-4553
dc.identifier.urihttp://hdl.handle.net/1885/54722
dc.publisherBirkhauser Verlag
dc.sourcePure and Applied Geophysics
dc.subjectKeywords: discrete element method; earthquake; fault; friction; micromechanics; shear; simulation; three-dimensional modeling Accelerating energy release; Discrete element method; Granular shear; Lattice solid model; Macroscopic friction; Parallel simulation
dc.titleParallel 3-D Simulation of a Fault Gouge Using the Lattice Solid Model
dc.typeJournal article
local.bibliographicCitation.issue9
local.bibliographicCitation.lastpage1964
local.bibliographicCitation.startpage1949
local.contributor.affiliationLatham, Shane, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationAbe, Steffen, University of Queensland
local.contributor.affiliationMora, Peter Ronald, University of Queensland
local.contributor.authoruidLatham, Shane, u3813363
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor020405 - Soft Condensed Matter
local.identifier.ariespublicationu9210271xPUB308
local.identifier.citationvolume163
local.identifier.doi10.1007/s00024-006-0106-2
local.identifier.scopusID2-s2.0-33750367159
local.type.statusPublished Version

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