Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction

Abstract The subduction of active spreading centers is an unusual phenomenon along subduction zones. In southern Chile, the Nazca‐Antarctic spreading system (Chile Rise) subducts beneath the South America plate at the Chile Triple Junction (CTJ), forming the Patagonian slab window. The beginning (sp...

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Main Authors: Kellen Azúa, Satoshi Ide, Seiya Yano, Sergio Ruiz, Hiroko Sugioka, Hajime Shiobara, Aki Ito, Matthew Miller, Hikaru Iwamori
Format: Article
Language:English
Published: Wiley 2025-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL115019
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author Kellen Azúa
Satoshi Ide
Seiya Yano
Sergio Ruiz
Hiroko Sugioka
Hajime Shiobara
Aki Ito
Matthew Miller
Hikaru Iwamori
author_facet Kellen Azúa
Satoshi Ide
Seiya Yano
Sergio Ruiz
Hiroko Sugioka
Hajime Shiobara
Aki Ito
Matthew Miller
Hikaru Iwamori
author_sort Kellen Azúa
collection DOAJ
description Abstract The subduction of active spreading centers is an unusual phenomenon along subduction zones. In southern Chile, the Nazca‐Antarctic spreading system (Chile Rise) subducts beneath the South America plate at the Chile Triple Junction (CTJ), forming the Patagonian slab window. The beginning (spatially youngest portion) of the slab window has been estimated based on plate kinematic reconstructions, but direct observations remain insufficient. To investigate this tectonic feature in detail, an Ocean Bottom Seismometer array was deployed south of the CTJ between 2019 and 2021. Using these continuous data and the envelope correlation method, we searched for tectonic tremors to complement the seismic observations and detected more than 500 events in this period. A notable separation between fast seismicity and tremors is observed at the current location of the subducted Chile Rise segment. We interpret this seismic gap as evidence of the Patagonian slab window formation within the last 0.3 Myr.
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language English
publishDate 2025-07-01
publisher Wiley
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series Geophysical Research Letters
spelling doaj-art-3561fa31937f4edaa820a9062c4e427f2025-08-20T02:46:20ZengWileyGeophysical Research Letters0094-82761944-80072025-07-015214n/an/a10.1029/2025GL115019Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple JunctionKellen Azúa0Satoshi Ide1Seiya Yano2Sergio Ruiz3Hiroko Sugioka4Hajime Shiobara5Aki Ito6Matthew Miller7Hikaru Iwamori8Departamento de Geofísica Universidad de Chile Santiago ChileDepartment of Earth and Planetary Science The University of Tokyo Tokyo JapanDepartment of Earth and Planetary Science The University of Tokyo Tokyo JapanDepartamento de Geofísica Universidad de Chile Santiago ChileKobe University Kobe JapanEarthquake Research Institute The University of Tokyo Tokyo JapanJapan Agency of Marine‐Earth Science and Technology Yokosuka JapanDepartamento de Geofísica Universidad de Concepción Concepción ChileEarthquake Research Institute The University of Tokyo Tokyo JapanAbstract The subduction of active spreading centers is an unusual phenomenon along subduction zones. In southern Chile, the Nazca‐Antarctic spreading system (Chile Rise) subducts beneath the South America plate at the Chile Triple Junction (CTJ), forming the Patagonian slab window. The beginning (spatially youngest portion) of the slab window has been estimated based on plate kinematic reconstructions, but direct observations remain insufficient. To investigate this tectonic feature in detail, an Ocean Bottom Seismometer array was deployed south of the CTJ between 2019 and 2021. Using these continuous data and the envelope correlation method, we searched for tectonic tremors to complement the seismic observations and detected more than 500 events in this period. A notable separation between fast seismicity and tremors is observed at the current location of the subducted Chile Rise segment. We interpret this seismic gap as evidence of the Patagonian slab window formation within the last 0.3 Myr.https://doi.org/10.1029/2025GL115019slab windowshallow tectonic tremorsmid‐ocean ridge
spellingShingle Kellen Azúa
Satoshi Ide
Seiya Yano
Sergio Ruiz
Hiroko Sugioka
Hajime Shiobara
Aki Ito
Matthew Miller
Hikaru Iwamori
Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
Geophysical Research Letters
slab window
shallow tectonic tremors
mid‐ocean ridge
title Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
title_full Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
title_fullStr Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
title_full_unstemmed Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
title_short Shallow Tectonic Tremors Reveal the Beginning of the Slab Window at the Chilean Triple Junction
title_sort shallow tectonic tremors reveal the beginning of the slab window at the chilean triple junction
topic slab window
shallow tectonic tremors
mid‐ocean ridge
url https://doi.org/10.1029/2025GL115019
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