namics The great majority of postglacial rebound computations carried out during the last three decades assumed a purely linear rheological relation for the mantle. Experimental data on high-temperature creep deformation and modelling of other tectonic processes, however, might also support the existence of non-linear creep mechanisms. We addressed postglacial rebound in North America through an axially symmetric finite-element model with a composite (linear plus non-linear) mantle rheology. In such a formulation, the transition stress σ T governs the balance between linear and non-linear creep components, while the term σ B, added to the effective shear stress, accounts for the background (ambient) stress induced by convection an...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...
namics The great majority of postglacial rebound computations carried out during the last three deca...
namics The great majority of postglacial rebound computations carried out during the last three deca...
In a previous work, cast in axisymmetric flat geometry, we have shown that a realistic composite rhe...
none2Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we ha...
Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we have pr...
Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we have pr...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...
namics The great majority of postglacial rebound computations carried out during the last three deca...
namics The great majority of postglacial rebound computations carried out during the last three deca...
In a previous work, cast in axisymmetric flat geometry, we have shown that a realistic composite rhe...
none2Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we ha...
Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we have pr...
Although studies on glacial isostatic adjustment usually assume a purely linear rheology, we have pr...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
Using finite-elements we study the postglacial rebound in an axisymmetric Earth with a non-Newtonian...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostati...