| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445038 | Journal of Structural Geology | 2013 | 13 Pages |
Abstract
⺠Examined microstructures of cm-scale faults in unlithified sands, silts and clays. ⺠Recognised two primary deformation mechanisms; granular shearing and cataclasis. ⺠Different shear band architectures are related to different deformation mechanisms. ⺠Deformation mechanisms and structures may relate to burial depth during faulting.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
M.B. Kristensen, C. Childs, N.Ã. Olesen, J.A. KorstgÃ¥rd,