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

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

2008-01-03

arxiv.org/abs/0801.0560v1

Tectonophysics 441 (2007) 47-65

Physics

Geophysics

Scientific paper

10.1016/j.tecto.2007.05.001

Theoretical 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.

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