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Mechanism of progressive broad deformation from oceanic transform valley to off-transform faulting and rifting
Oceanic transform faults (TFs) are commonly viewed as single, narrow strike-slip seismic faults that offset two mid-ocean ridge segments. However, broad zones of complex deformation are ubiquitous at TFs. Here, we propose a new conceptual model for the progressive deformation within broad zones at o...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Elsevier
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8693269/ https://www.ncbi.nlm.nih.gov/pubmed/34984410 http://dx.doi.org/10.1016/j.xinn.2021.100193 |