| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9528380 | Tectonophysics | 2018 | 46 Pages |
Abstract
In TF1, while the major mineralogical changes occur in the damage zone. In ASM1, a higher illite-smectite mixed layers and calcite content was observed in the eastern side of the fault.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Eva Moreno, Catherine Homberg, Johann Schnyder, Alain Person, Christian David, Arthur du Peloux, Emeline Moubeche, Audrey Bonnelye, Pierre Dick,