Melting of subducted sediments reconciles geophysical images of subduction zones
Here, the authors identify that magnetotelluric conductive anomalies commonly observed on the trenchward-side of volcanic arcs in subduction zones can be explained by subducted sediments. High-pressure experiments show that these sediment melts will react with the overlying mantle wedge to produce e...
Guardado en:
Autores principales: | , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/86e1e86e7dab4aec9259af27d6754f95 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:86e1e86e7dab4aec9259af27d6754f95 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:86e1e86e7dab4aec9259af27d6754f952021-12-02T13:32:50ZMelting of subducted sediments reconciles geophysical images of subduction zones10.1038/s41467-021-21657-82041-1723https://doaj.org/article/86e1e86e7dab4aec9259af27d6754f952021-02-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-21657-8https://doaj.org/toc/2041-1723Here, the authors identify that magnetotelluric conductive anomalies commonly observed on the trenchward-side of volcanic arcs in subduction zones can be explained by subducted sediments. High-pressure experiments show that these sediment melts will react with the overlying mantle wedge to produce electrically conductive phlogopite pyroxenites.M. W. FörsterK. SelwayNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-7 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q M. W. Förster K. Selway Melting of subducted sediments reconciles geophysical images of subduction zones |
description |
Here, the authors identify that magnetotelluric conductive anomalies commonly observed on the trenchward-side of volcanic arcs in subduction zones can be explained by subducted sediments. High-pressure experiments show that these sediment melts will react with the overlying mantle wedge to produce electrically conductive phlogopite pyroxenites. |
format |
article |
author |
M. W. Förster K. Selway |
author_facet |
M. W. Förster K. Selway |
author_sort |
M. W. Förster |
title |
Melting of subducted sediments reconciles geophysical images of subduction zones |
title_short |
Melting of subducted sediments reconciles geophysical images of subduction zones |
title_full |
Melting of subducted sediments reconciles geophysical images of subduction zones |
title_fullStr |
Melting of subducted sediments reconciles geophysical images of subduction zones |
title_full_unstemmed |
Melting of subducted sediments reconciles geophysical images of subduction zones |
title_sort |
melting of subducted sediments reconciles geophysical images of subduction zones |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doaj.org/article/86e1e86e7dab4aec9259af27d6754f95 |
work_keys_str_mv |
AT mwforster meltingofsubductedsedimentsreconcilesgeophysicalimagesofsubductionzones AT kselway meltingofsubductedsedimentsreconcilesgeophysicalimagesofsubductionzones |
_version_ |
1718392865740029952 |