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Volcanism in slab tear faults is larger than in island-arcs and back-arcs

Subduction-transform edge propagators are lithospheric tears bounding slabs and back-arc basins. The volcanism at these edges is enigmatic because it is lacking comprehensive geological and geophysical data. Here we present bathymetric, potential-field data, and direct observations of the seafloor o...

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Detalles Bibliográficos
Autores principales: Cocchi, Luca, Passaro, Salvatore, Tontini, Fabio Caratori, Ventura, Guido
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5682279/
https://www.ncbi.nlm.nih.gov/pubmed/29129913
http://dx.doi.org/10.1038/s41467-017-01626-w