Asperity interactions during creep of simulated faults at hydrothermal conditions

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dc.contributor.authorStreit, J
dc.contributor.authorCox, Stephen
dc.date.accessioned2015-12-13T23:18:24Z
dc.date.available2015-12-13T23:18:24Z
dc.date.issued2000
dc.date.updated2015-12-12T08:56:37Z
dc.description.abstractGrain-scale deformation processes during sliding on simulated faults, and in the presence of reactive pore fluids, are examined with in situ, see-through experiments using polycrystalline biphenyl aggregates at 60 °C as a rock analogue. Reactive pore flu
dc.identifier.issn0091-7613
dc.identifier.urihttp://hdl.handle.net/1885/90156
dc.publisherGeological Society of America Inc
dc.sourceGeology
dc.subjectKeywords: Asperity shearing; Crack propagation; Crystal growth; Deformation; Dissolution; Fracture; Friction; Polycrystalline materials; Porosity; Precipitation (chemical); Rock mechanics; Tectonics
dc.titleAsperity interactions during creep of simulated faults at hydrothermal conditions
dc.typeJournal article
local.bibliographicCitation.lastpage234
local.bibliographicCitation.startpage231
local.contributor.affiliationStreit, J, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationCox, Stephen, College of Physical and Mathematical Sciences, ANU
local.contributor.authoremailu8410159@anu.edu.au
local.contributor.authoruidStreit, J, u3748643
local.contributor.authoruidCox, Stephen, u8410159
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040312 - Structural Geology
local.identifier.ariespublicationMigratedxPub20444
local.identifier.citationvolume28
local.identifier.scopusID2-s2.0-0034351122
local.identifier.uidSubmittedByMigrated
local.type.statusPublished Version

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