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...

Descripción completa

Detalles Bibliográficos
Autores principales: Zhang, Fan, Lin, Jian, Zhou, Zhiyuan, Yang, Hongfeng, Morgan, Jason P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2021
Materias:
Report
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

Internet

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

Ejemplares similares