| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4694971 | Tectonophysics | 2006 | 15 Pages |
Abstract
These results differ fundamentally from purely physical models of ductile flow around a rigid object and demonstrate the influence of interface diffusional properties on the resulting behaviour. In particular, assumptions such as perturbation of the flow by the object, deflection of external foliation around pre-deformational porphyroblasts and relationships of pressure-shadow strain to bulk strain may need to be re-examined in the light of this finding.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
J.R. Berton, D.W. Durney, J. Wheeler, J.M. Ford,