A first order interpretation of deformation at a volcano is often one of a change in volume within a long-lived magma chamber or reservoir (which could be loosely defined as a site of repeated intrusion).
Strain transfer between the two orientations leads to complex stress/strain states, hindering interpretations of plastic deformation behaviors such as strain hardening and anelasticity.
The present simulations thus give further encouragement to interpretations of chain deformations in filled systems in terms of volume exclusion effects from the nanoparticle inclusions, including their dispersions and arrangements within polymer matrices.
The detection of strain anomalies in the coseismic period enables a new interpretation of the deformation process at strain concentration zones.
We do not attempt to separate out data from magmatic and hydrothermal sources here, but note the authors' interpretation of the deformation.
Field-based interpretation of ground deformation in rock glaciers and movements in talus slopes correlates well with the ratio of InSAR images showing potential ground deformation.
Making corotational rates associated with specific spin tensors is a matter of interest, which can help for a better physical interpretation of the deformation.
The objective of this study is to provide interpretation of the deformation modes in the finite element absolute nodal coordinate formulation using several strain definitions.
This process also enables high-density four-dimensional strain mapping by tracking particles located in grains, providing direct interpretation of localized deformation caused by interaction between neighbouring grains.
The manuscript describes and compares data sets and normalizing procedures for these variables, in order to choose a suitable set that facilitates the interpretation of the deformation, as well as the comparison between the outputs of different die designs.
