Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction

The Southern Atlantic-Southwest Indian ridges (SASWIR) host mid-ocean ridge basalts with a residual subduction-related geochemical fingerprint (i.e., a ghost-arc signature) of unclear origin. Here, we show through an analysis of plate kinematic reconstructions and seismic tomography models that the...

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Published in:Nature Communications
Main Authors: Gianni, Guido Martin, Likerman, Jeremias, Navarrete Granzotto, César Rodrigo, Gianni, Conrado Rubén, Zlotnik, Sergio
Format: Article in Journal/Newspaper
Language:English
Published: Nature
Subjects:
Online Access:http://hdl.handle.net/11336/218426
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author Gianni, Guido Martin
Likerman, Jeremias
Navarrete Granzotto, César Rodrigo
Gianni, Conrado Rubén
Zlotnik, Sergio
author_facet Gianni, Guido Martin
Likerman, Jeremias
Navarrete Granzotto, César Rodrigo
Gianni, Conrado Rubén
Zlotnik, Sergio
author_sort Gianni, Guido Martin
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 1
container_title Nature Communications
container_volume 14
description The Southern Atlantic-Southwest Indian ridges (SASWIR) host mid-ocean ridge basalts with a residual subduction-related geochemical fingerprint (i.e., a ghost-arc signature) of unclear origin. Here, we show through an analysis of plate kinematic reconstructions and seismic tomography models that the SASWIR subduction-modified mantle source formed in the Jurassic close to the Georgia Islands slab (GI) and remained near-stationary in the mantle reference frame. In this analysis, the GI lies far inboard the Jurassic Patagonian-Antarctic Peninsula active margin. This was formerly attributed to a large-scale flat subduction event in the Late Triassic-Early Jurassic. We propose that during this flat slab stage, the subduction-modified mantle areas beneath the Mesozoic active margin and surrounding sutures zones may have been bulldozed inland by >2280 km. After the demise of the flat slab, this mantle anomaly remained near-stationary and was sampled by the Karoo mantle plume 183 Million years (Myr) ago and again since 55 Myr ago by the SASWIR. We refer to this process as asthenospheric anomaly telescoping. This study provides a hitherto unrecognized geodynamic effect of flat subduction, the viability of which we support through numerical modeling. Fil: Gianni, Guido Martin. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan; Argentina Fil: Likerman, Jeremias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y ...
format Article in Journal/Newspaper
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Antarctic
Antarctic Peninsula
genre_facet Antarc*
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Antarctic Peninsula
geographic Antarctic
Antarctic Peninsula
Argentina
Guido
Indian
Navarrete
Pablo
Patagonia
San Juan
geographic_facet Antarctic
Antarctic Peninsula
Argentina
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Indian
Navarrete
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/218426 2025-01-16T19:42:07+00:00 Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction Gianni, Guido Martin Likerman, Jeremias Navarrete Granzotto, César Rodrigo Gianni, Conrado Rubén Zlotnik, Sergio application/pdf http://hdl.handle.net/11336/218426 eng eng Nature info:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/s41467-023-37799-w info:eu-repo/semantics/altIdentifier/doi/10.1038/s41467-023-37799-w http://hdl.handle.net/11336/218426 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ghost-arc flat slab subduction SASWIR https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1038/s41467-023-37799-w 2024-10-04T09:34:11Z The Southern Atlantic-Southwest Indian ridges (SASWIR) host mid-ocean ridge basalts with a residual subduction-related geochemical fingerprint (i.e., a ghost-arc signature) of unclear origin. Here, we show through an analysis of plate kinematic reconstructions and seismic tomography models that the SASWIR subduction-modified mantle source formed in the Jurassic close to the Georgia Islands slab (GI) and remained near-stationary in the mantle reference frame. In this analysis, the GI lies far inboard the Jurassic Patagonian-Antarctic Peninsula active margin. This was formerly attributed to a large-scale flat subduction event in the Late Triassic-Early Jurassic. We propose that during this flat slab stage, the subduction-modified mantle areas beneath the Mesozoic active margin and surrounding sutures zones may have been bulldozed inland by >2280 km. After the demise of the flat slab, this mantle anomaly remained near-stationary and was sampled by the Karoo mantle plume 183 Million years (Myr) ago and again since 55 Myr ago by the SASWIR. We refer to this process as asthenospheric anomaly telescoping. This study provides a hitherto unrecognized geodynamic effect of flat subduction, the viability of which we support through numerical modeling. Fil: Gianni, Guido Martin. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan; Argentina Fil: Likerman, Jeremias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Antarctic Peninsula Argentina Guido ENVELOPE(-60.933,-60.933,-64.050,-64.050) Indian Navarrete ENVELOPE(-62.533,-62.533,-64.833,-64.833) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Patagonia San Juan Nature Communications 14 1
spellingShingle ghost-arc
flat slab
subduction
SASWIR
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Gianni, Guido Martin
Likerman, Jeremias
Navarrete Granzotto, César Rodrigo
Gianni, Conrado Rubén
Zlotnik, Sergio
Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title_full Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title_fullStr Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title_full_unstemmed Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title_short Ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
title_sort ghost-arc geochemical anomaly at a spreading ridge caused by supersized flat subduction
topic ghost-arc
flat slab
subduction
SASWIR
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet ghost-arc
flat slab
subduction
SASWIR
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/218426