| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445094 | Journal of Structural Geology | 2012 | 14 Pages |
Abstract
⺠The morphology of the Dixie Valley fault has been measured in 3D. ⺠The fault slip surface is characterized by a fractal geometry. ⺠This geometry is explained by the formation of lenses of damaged material. ⺠A geometrical correlation exists between the slip surface and the damaged zone. âºÂ This correlation is explained through a mechanical model.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Thibault Candela, François Renard,