Abstract
Simple governing equations coupling diffusional transport at a macroscopic scale and deformation in a tight rock are formulated. The deformation alone is described by a linear viscous rheology. Several deformations of geological interest are analyzed, including the folding of an embedded layer. A basic feature is the length-scale dependence of diffusional effects. Interpretation of natural structures permits the estimation of parameters governing the diffusional transport and rate of deformation.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 275-291 |
| Number of pages | 17 |
| Journal | Tectonophysics |
| Volume | 83 |
| Issue number | 3-4 |
| DOIs | |
| State | Published - Mar 20 1982 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Earth-Surface Processes
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