Résumé
Why are strike slip faults not perfectly linear but made of successive segments? Are they reminiscences of the fracture of an initially sound crust by the bottom-up propagation of a crack subjected to mode III loading? The plausibility of this newly proposed scenario will be investigated here through model experiments and some theoretical explanations in the framework of brittle fracture.
| langue originale | Anglais |
|---|---|
| Numéro d'article | 20170392 |
| journal | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
| Volume | 377 |
| Numéro de publication | 2136 |
| Les DOIs | |
| état | Publié - 14 janv. 2019 |
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