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Nanocrystalline Principal Slip Zones and Their Role in Controlling Crustal Fault Rheology
Principal slip zones (PSZs) are narrow (<10 cm) bands of localized shear deformation that occur in the cores of upper-crustal fault zones where they accommodate the bulk of fault displacement. Natural and experimentally-formed PSZs consistently show the presence of nanocrystallites in the &am...
Tallennettuna:
| Päätekijät: | , , |
|---|---|
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
MDPI AG
2019-05-01
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| Sarja: | Minerals |
| Aiheet: | |
| Linkit: | https://www.mdpi.com/2075-163X/9/6/328 |
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