Cargando…
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...
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 |
Ejemplares similares
-
Slab to back-arc to arc: Fluid and melt pathways through the mantle wedge beneath the Lesser Antilles
por: Hicks, Stephen P., et al.
Publicado: (2023) -
Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
por: Bénard, Antoine, et al.
Publicado: (2018) -
Fault-controlled deep hydrothermal flow in a back-arc tectonic setting, SE Tyrrhenian Sea
por: Loreto, Maria Filomena, et al.
Publicado: (2019) -
Climatic control on the location of continental volcanic arcs
por: Muller, Veleda A. P., et al.
Publicado: (2022) -
Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge
por: De Pascale, Gregory P., et al.
Publicado: (2021)