| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445097 | Journal of Structural Geology | 2012 | 12 Pages |
Abstract
⺠Fault zone microstructures are described by two different scaling properties. ⺠We use H (fracture surface roughness) and D (grain size distribution). ⺠Grain size distribution: D increases with proximity to shear zone centres. ⺠Fracture roughness: data set described satisfactorily by single mean value. ⺠Further work: closer analysis of H and D relation at shear zone edges.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Hilary Dyer, David Amitrano, Anne-Marie Boullier,