Field‐Based Evidence for Intra‐Slab High‐Permeability Channel Formation at Eclogite‐Facies Conditions During Subduction

Fluid release from subducting oceanic lithosphere is a key process for subduction zone geodynamics, from controlling arc volcanism to seismicity and tectonic exhumation. However, many fundamental details of fluid composition, flow pathways, and reactivity with slab‐forming rocks remain to be thoroug...

Descripción completa

Detalles Bibliográficos
Autores principales: Piccoli, Francesca, Ague, Jay J., Chu, Xu, Tian, Meng, Vitale Brovarone, Alberto
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8047908/
https://www.ncbi.nlm.nih.gov/pubmed/33867865
http://dx.doi.org/10.1029/2020GC009520

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8047908/
https://www.ncbi.nlm.nih.gov/pubmed/33867865
http://dx.doi.org/10.1029/2020GC009520

Ejemplares similares