Influence of time, temperature, confining pressure and fluid content on the experimental compaction of spherical grains

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dc.creatorRossi, Magali
dc.creatorVidal, Olivier
dc.creatorWunder, Bernd
dc.creatorRenard, François
dc.date2008-01-03
dc.date.accessioned2026-07-07T08:52:23Z
dc.date.available2026-07-07T08:52:23Z
dc.descriptionTheoretical models of compaction processes, such as for example intergranular pressure-solution (IPS), focus on deformation occurring at the contacts between spherical grains that constitute an aggregate. In order to investigate the applicability of such models, and to quantify the deformation of particles within an aggregate, isostatic experiments were performed in cold-sealed vessels on glass sphere aggregates at 200 MPa confining pressure and 350 degrees C with varying amounts of fluid.
dc.identifierhttps://arxiv.org/abs/0801.0560
dc.identifierhttp://arxiv.org/abs/0801.0560
dc.identifierTectonophysics 441 (2007) 47-65
dc.identifierdoi:10.1016/j.tecto.2007.05.001
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/145262
dc.subjectGeophysics
dc.titleInfluence of time, temperature, confining pressure and fluid content on the experimental compaction of spherical grains
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