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Post-seismic stress relaxation with a linear transient rheology
Transient rheology Geodynamics Stress tensor Coulomb failure function Post-seismic relaxation
2015/8/28
We performed an analysis of post-seismic stress relaxation, taking into account generalized linear rheologies. We compared the stress field (and its derived functions) obtained with a classical Maxwel...
Cooling of a channeled lava flow with non-Newtonian rheology: crust formation and surface radiance
Rheology Magmas Thermodynamics Lava flow Effusion rate
2015/8/27
We present here the results from dynamical and thermal models that describe a channeled lava flow as it cools by radiation. In particular, the effects of power-law rheology and of the presence of bend...
Landslide velocity, thickness, and rheology from remote sensing: La Clapière landslide, France
Landslide velocity thickness rheology from remote sensing La Clapière landslide France
2014/4/8
Quantifying the velocity, volume, and rheology of deep,slow-moving landslides is essential for hazard prediction and understanding landscape evolution, but existing field-based methods are difficult o...
Constraints from rocks in the Taiwan orogen on crustal stress levels and rheology
rocks in the Taiwan orogen on crustal stress levels rheology
2014/4/15
Taiwan’s Hsüehshan range experienced penetrative coaxial deformation within and near the brittle-plastic transition between6.5 and 3 Ma. This recent and short-lasting deformation in an active, well-s...
Influence of Non-Newtonian rheology on magma degassing
Non-Newtonian rheology magma degassing Soft Condensed Matter
2011/8/4
Abstract: Many volcanoes exhibit temporal changes in their degassing process, from rapid gas puffing to lava fountaining and long-lasting quiescent passive degassing periods. This range of behaviors h...
Shear Flow of Sea Ice in the Marginal Ice Zone with Collision Rheology
Flow of Sea Ice Marginal Ice Zone Collision Rheology.
2009/6/15
Shear Flow of Sea Ice in the Marginal Ice Zone with Collision Rheology.