Microseismicity and lithosphere thickness at a nearly-amagmatic oceanic detachment fault system

Oceanic detachment faults play a central role in accommodating the plate divergence at slow-ultraslow spreading mid-ocean ridges. Successive flip-flop detachment faults in a nearly-amagmatic region of the ultraslow spreading Southwest Indian Ridge (SWIR) at 64°30’E accommodate ~100% of plate diverge...

Descripción completa

Detalles Bibliográficos
Autores principales: Chen, Jie, Crawford, Wayne C., Cannat, Mathilde
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9879945/
https://www.ncbi.nlm.nih.gov/pubmed/36702818
http://dx.doi.org/10.1038/s41467-023-36169-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9879945/
https://www.ncbi.nlm.nih.gov/pubmed/36702818
http://dx.doi.org/10.1038/s41467-023-36169-w

Ejemplares similares