Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography
- Autores
- Rodríguez, Emily E.; Portner, Daniel Evan; Beck, Susan L.; Rocha, Marcelo P.; Bianchi, Marcelo B.; Assumpção, Marcelo; Ruiz, Mario; Alvarado, Patricia Monica; Condori, Cristobal; Lynner, Colton
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Andean Subduction Zone is one of the longest continuous subduction zones on Earth. The relative simplicity of the two-plate system has makes it an ideal natural laboratory to study the dynamics in subduction zones. We measure teleseismic S and SKS traveltime residuals at >1000 seismic stations that have been deployed across South America over the last 30 yr to produce a finite-frequency teleseismic S-wave tomography model of the mantle beneath the Andean Subduction Zone related to the Nazca Plate, spanning from ~5°N to 45°S and from depths of ~130 to 1200 km. Within our model, the subducted Nazca slab is imaged as a fast velocity seismic anomaly. The geometry and amplitude of the Nazca slab anomaly varies along the margin while the slab anomaly continues into the lower mantle along the entirety of the subduction margin. Beneath northern Brazil, the Nazca slab appears to stagnate at ~1000 km depth and extend eastward subhorizontally for >2000 km. South of 25°S the slab anomaly in the lower mantle extends offshore of eastern Argentina, hence we do not image if a similar stagnation occurs. We image several distinct features surrounding the slab including two vertically oriented slow seismic velocity anomalies: one beneath the Peruvian flat slab and the other beneath the Paraná Basin of Brazil. The presence of the latter anomaly directly adjacent to the stagnant Nazca slab suggests that the plume, known as the Paraná Plume, may be a focused upwelling formed in response to slab stagnation in the lower mantle. Additionally, we image a high amplitude fast seismic velocity anomaly beneath the Chile trench at the latitude of the Sierras Pampeanas which extends from ~400 to ~1000 km depth. This anomaly may be the remnants of an older, detached slab, however its relationship with the Nazca-South America subduction zone remains enigmatic.
Fil: Rodríguez, Emily E.. University of Arizona; Estados Unidos
Fil: Portner, Daniel Evan. No especifíca;
Fil: Beck, Susan L.. University of Arizona; Estados Unidos
Fil: Rocha, Marcelo P.. Universidade do Brasília; Brasil
Fil: Bianchi, Marcelo B.. Universidade de Sao Paulo; Brasil
Fil: Assumpção, Marcelo. Universidade de Sao Paulo; Brasil
Fil: Ruiz, Mario. Escuela Politécnica Nacional; Ecuador
Fil: Alvarado, Patricia Monica. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geofísica y Astronomía; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan. Centro de Investigaciones de la Geosfera y Biosfera. Universidad Nacional de San Juan. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones de la Geosfera y Biosfera; Argentina
Fil: Condori, Cristobal. Universidade do Brasília; Brasil
Fil: Lynner, Colton. University Of Delaware; Estados Unidos - Materia
-
DYNAMICS OF LITHOSPHERE AND MANTLE
SEISMIC TOMOGRAPHY
SOUTH AMERICA - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/183354
Ver los metadatos del registro completo
id |
CONICETDig_c20b4554ac35194b89ef9d9cb7539a89 |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/183354 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
spelling |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomographyRodríguez, Emily E.Portner, Daniel EvanBeck, Susan L.Rocha, Marcelo P.Bianchi, Marcelo B.Assumpção, MarceloRuiz, MarioAlvarado, Patricia MonicaCondori, CristobalLynner, ColtonDYNAMICS OF LITHOSPHERE AND MANTLESEISMIC TOMOGRAPHYSOUTH AMERICAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Andean Subduction Zone is one of the longest continuous subduction zones on Earth. The relative simplicity of the two-plate system has makes it an ideal natural laboratory to study the dynamics in subduction zones. We measure teleseismic S and SKS traveltime residuals at >1000 seismic stations that have been deployed across South America over the last 30 yr to produce a finite-frequency teleseismic S-wave tomography model of the mantle beneath the Andean Subduction Zone related to the Nazca Plate, spanning from ~5°N to 45°S and from depths of ~130 to 1200 km. Within our model, the subducted Nazca slab is imaged as a fast velocity seismic anomaly. The geometry and amplitude of the Nazca slab anomaly varies along the margin while the slab anomaly continues into the lower mantle along the entirety of the subduction margin. Beneath northern Brazil, the Nazca slab appears to stagnate at ~1000 km depth and extend eastward subhorizontally for >2000 km. South of 25°S the slab anomaly in the lower mantle extends offshore of eastern Argentina, hence we do not image if a similar stagnation occurs. We image several distinct features surrounding the slab including two vertically oriented slow seismic velocity anomalies: one beneath the Peruvian flat slab and the other beneath the Paraná Basin of Brazil. The presence of the latter anomaly directly adjacent to the stagnant Nazca slab suggests that the plume, known as the Paraná Plume, may be a focused upwelling formed in response to slab stagnation in the lower mantle. Additionally, we image a high amplitude fast seismic velocity anomaly beneath the Chile trench at the latitude of the Sierras Pampeanas which extends from ~400 to ~1000 km depth. This anomaly may be the remnants of an older, detached slab, however its relationship with the Nazca-South America subduction zone remains enigmatic.Fil: Rodríguez, Emily E.. University of Arizona; Estados UnidosFil: Portner, Daniel Evan. No especifíca;Fil: Beck, Susan L.. University of Arizona; Estados UnidosFil: Rocha, Marcelo P.. Universidade do Brasília; BrasilFil: Bianchi, Marcelo B.. Universidade de Sao Paulo; BrasilFil: Assumpção, Marcelo. Universidade de Sao Paulo; BrasilFil: Ruiz, Mario. Escuela Politécnica Nacional; EcuadorFil: Alvarado, Patricia Monica. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geofísica y Astronomía; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan. Centro de Investigaciones de la Geosfera y Biosfera. Universidad Nacional de San Juan. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones de la Geosfera y Biosfera; ArgentinaFil: Condori, Cristobal. Universidade do Brasília; BrasilFil: Lynner, Colton. University Of Delaware; Estados UnidosWiley Blackwell Publishing, Inc2021-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/183354Rodríguez, Emily E.; Portner, Daniel Evan; Beck, Susan L.; Rocha, Marcelo P.; Bianchi, Marcelo B.; et al.; Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography; Wiley Blackwell Publishing, Inc; Geophysical Journal International; 224; 3; 3-2021; 1553-15710956-540XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1093/gji/ggaa536info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:40:31Zoai:ri.conicet.gov.ar:11336/183354instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:40:31.98CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
title |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
spellingShingle |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography Rodríguez, Emily E. DYNAMICS OF LITHOSPHERE AND MANTLE SEISMIC TOMOGRAPHY SOUTH AMERICA |
title_short |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
title_full |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
title_fullStr |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
title_full_unstemmed |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
title_sort |
Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography |
dc.creator.none.fl_str_mv |
Rodríguez, Emily E. Portner, Daniel Evan Beck, Susan L. Rocha, Marcelo P. Bianchi, Marcelo B. Assumpção, Marcelo Ruiz, Mario Alvarado, Patricia Monica Condori, Cristobal Lynner, Colton |
author |
Rodríguez, Emily E. |
author_facet |
Rodríguez, Emily E. Portner, Daniel Evan Beck, Susan L. Rocha, Marcelo P. Bianchi, Marcelo B. Assumpção, Marcelo Ruiz, Mario Alvarado, Patricia Monica Condori, Cristobal Lynner, Colton |
author_role |
author |
author2 |
Portner, Daniel Evan Beck, Susan L. Rocha, Marcelo P. Bianchi, Marcelo B. Assumpção, Marcelo Ruiz, Mario Alvarado, Patricia Monica Condori, Cristobal Lynner, Colton |
author2_role |
author author author author author author author author author |
dc.subject.none.fl_str_mv |
DYNAMICS OF LITHOSPHERE AND MANTLE SEISMIC TOMOGRAPHY SOUTH AMERICA |
topic |
DYNAMICS OF LITHOSPHERE AND MANTLE SEISMIC TOMOGRAPHY SOUTH AMERICA |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Andean Subduction Zone is one of the longest continuous subduction zones on Earth. The relative simplicity of the two-plate system has makes it an ideal natural laboratory to study the dynamics in subduction zones. We measure teleseismic S and SKS traveltime residuals at >1000 seismic stations that have been deployed across South America over the last 30 yr to produce a finite-frequency teleseismic S-wave tomography model of the mantle beneath the Andean Subduction Zone related to the Nazca Plate, spanning from ~5°N to 45°S and from depths of ~130 to 1200 km. Within our model, the subducted Nazca slab is imaged as a fast velocity seismic anomaly. The geometry and amplitude of the Nazca slab anomaly varies along the margin while the slab anomaly continues into the lower mantle along the entirety of the subduction margin. Beneath northern Brazil, the Nazca slab appears to stagnate at ~1000 km depth and extend eastward subhorizontally for >2000 km. South of 25°S the slab anomaly in the lower mantle extends offshore of eastern Argentina, hence we do not image if a similar stagnation occurs. We image several distinct features surrounding the slab including two vertically oriented slow seismic velocity anomalies: one beneath the Peruvian flat slab and the other beneath the Paraná Basin of Brazil. The presence of the latter anomaly directly adjacent to the stagnant Nazca slab suggests that the plume, known as the Paraná Plume, may be a focused upwelling formed in response to slab stagnation in the lower mantle. Additionally, we image a high amplitude fast seismic velocity anomaly beneath the Chile trench at the latitude of the Sierras Pampeanas which extends from ~400 to ~1000 km depth. This anomaly may be the remnants of an older, detached slab, however its relationship with the Nazca-South America subduction zone remains enigmatic. Fil: Rodríguez, Emily E.. University of Arizona; Estados Unidos Fil: Portner, Daniel Evan. No especifíca; Fil: Beck, Susan L.. University of Arizona; Estados Unidos Fil: Rocha, Marcelo P.. Universidade do Brasília; Brasil Fil: Bianchi, Marcelo B.. Universidade de Sao Paulo; Brasil Fil: Assumpção, Marcelo. Universidade de Sao Paulo; Brasil Fil: Ruiz, Mario. Escuela Politécnica Nacional; Ecuador Fil: Alvarado, Patricia Monica. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geofísica y Astronomía; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan. Centro de Investigaciones de la Geosfera y Biosfera. Universidad Nacional de San Juan. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones de la Geosfera y Biosfera; Argentina Fil: Condori, Cristobal. Universidade do Brasília; Brasil Fil: Lynner, Colton. University Of Delaware; Estados Unidos |
description |
The Andean Subduction Zone is one of the longest continuous subduction zones on Earth. The relative simplicity of the two-plate system has makes it an ideal natural laboratory to study the dynamics in subduction zones. We measure teleseismic S and SKS traveltime residuals at >1000 seismic stations that have been deployed across South America over the last 30 yr to produce a finite-frequency teleseismic S-wave tomography model of the mantle beneath the Andean Subduction Zone related to the Nazca Plate, spanning from ~5°N to 45°S and from depths of ~130 to 1200 km. Within our model, the subducted Nazca slab is imaged as a fast velocity seismic anomaly. The geometry and amplitude of the Nazca slab anomaly varies along the margin while the slab anomaly continues into the lower mantle along the entirety of the subduction margin. Beneath northern Brazil, the Nazca slab appears to stagnate at ~1000 km depth and extend eastward subhorizontally for >2000 km. South of 25°S the slab anomaly in the lower mantle extends offshore of eastern Argentina, hence we do not image if a similar stagnation occurs. We image several distinct features surrounding the slab including two vertically oriented slow seismic velocity anomalies: one beneath the Peruvian flat slab and the other beneath the Paraná Basin of Brazil. The presence of the latter anomaly directly adjacent to the stagnant Nazca slab suggests that the plume, known as the Paraná Plume, may be a focused upwelling formed in response to slab stagnation in the lower mantle. Additionally, we image a high amplitude fast seismic velocity anomaly beneath the Chile trench at the latitude of the Sierras Pampeanas which extends from ~400 to ~1000 km depth. This anomaly may be the remnants of an older, detached slab, however its relationship with the Nazca-South America subduction zone remains enigmatic. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-03 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/183354 Rodríguez, Emily E.; Portner, Daniel Evan; Beck, Susan L.; Rocha, Marcelo P.; Bianchi, Marcelo B.; et al.; Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography; Wiley Blackwell Publishing, Inc; Geophysical Journal International; 224; 3; 3-2021; 1553-1571 0956-540X CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/183354 |
identifier_str_mv |
Rodríguez, Emily E.; Portner, Daniel Evan; Beck, Susan L.; Rocha, Marcelo P.; Bianchi, Marcelo B.; et al.; Mantle dynamics of the Andean Subduction Zone from continent-scale teleseismic S-wave tomography; Wiley Blackwell Publishing, Inc; Geophysical Journal International; 224; 3; 3-2021; 1553-1571 0956-540X CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1093/gji/ggaa536 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Wiley Blackwell Publishing, Inc |
publisher.none.fl_str_mv |
Wiley Blackwell Publishing, Inc |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
_version_ |
1844614433589952512 |
score |
13.070432 |