Sentence examples for source deformation from inspiring English sources

Deep source deformation (node 1) is a latent node with moderate potential to influence eruption probability.

These apparently contradictory results are explained on the basis of source limited deformation.

The basic idea was to use the connectors as the main source of deformation and energy dissipation, and to realize rapid repair of the joints by simple replacement of theses connectors after earthquakes.

The source of deformation is related to a depressurisation of the system that results from the release of magmatic fluids across the boundary between the brittle and plastic domains.

Deep source ground deformation.

This pattern can result from a second source of deformation.

This is a simple binary node – the state is either true or false.   1 Deep source ground deformation.

In the apical region with strong volume source, the deformation of the nearby tissues is large and the neighborhood relationship among cells is easy to change (i.e., the plasticity of tissue).

We then used these three sources of deformation to initialise a nonlinear inversion of the surface deformation that takes the six displacement fields as an input (InSAR, SAR range offset and SAR azimuth offset, for ascending and descending passes).

Inelastic lithostatic compaction (P*) can occur far from the sources of deformation but requires depths of at least 4 5 km (although we note that very porous rocks—such as pumiceous or scoracious rocks (see Farquharson et al. 2015)—may encounter inelastic lithostatic compaction at volcanologically relevant depths).

Among these candidates of simple deformation source, spherical and vertical pipe sources were excluded because these sources produce only axisymmetric surface deformation.