Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina

Autores
Godoy, Laura B.; Nacif, Silvina; Lupari, Marianela; García, Héctor P. A.; Correa-Otto, Sebastián; Melchor, Iván; Pechuan, Stefanie N.; Ariza, Juan P.; Gimenez, Mario Ernesto; Caselli, Alberto Tomás
Año de publicación
2020
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Fil: Godoy, Laura. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Nacif, Silvina. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Lupari, Marianela. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: García, Héctor. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Correa-Otto, Sebastián. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Melchor, Iván. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.
Fil: Pechuan, Stefanie. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Ariza, Juan. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Gimenez, Mario Ernesto. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Caselli, Alberto. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.
Cerro Domuyo, in northwestern Neuquén province of Argentina, shows notable geothermal activity, although it is located at a considerable distance from the actual volcanic arc. Many studies have been developed in this area with the aim of investigating its geothermal field. Despite these efforts, the characterization of the dynamic activity in the area is still poorly known. This work shows the results of a network of seismological stations, which registered volcano-tectonic, long-period and hybrid events. A large number of volcano-tectonic events concentrated mostly in the Cerro Domuyo geothermal area were detected. These events can be divided into two groups, those that occurred at shallow depths below the geothermal area and those at greater depths below the high region of Cerro Domuyo. Shallow events were located around the Manchana Covunco fault and many of them were particularly clustered at its intersection with the Humazo fault. Seismicity in the area shows that these faults are continually active due to fluid movement, as was evidenced by the hydrothermal manifestation of the Humazo in 2003. Moreover, new studies provide evidence that the Cerro Domuyo is experiencing an important inflation caused by a magmatic body. Deep volcano-tectonic events are evidencing this activity. Considering the large distance between the actual volcanic arc and the study region, and the high density of shallow volcano-tectonic events, it is highly likely that this magmatic body is increasing the geothermal activity. Additionally, the aeromagnetic anomaly over Cerro Domuyo is showing a thin magnetic crust of less than 6 km, suggesting a clear link between the geophysical results and the inflation in Cerro Domuyo.
.
Materia
Ciencias Exactas y Naturales
Volcanism
Domuyo
Geothermal Field
Micro Seismicity
Thermal Anomaly
Ciencias Exactas y Naturales
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
RID-UNRN (UNRN)
Institución
Universidad Nacional de Río Negro
OAI Identificador
oai:rid.unrn.edu.ar:20.500.12049/7384

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repository_id_str 4369
network_name_str RID-UNRN (UNRN)
spelling Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, ArgentinaGodoy, Laura B.Nacif, SilvinaLupari, MarianelaGarcía, Héctor P. A.Correa-Otto, SebastiánMelchor, IvánPechuan, Stefanie N.Ariza, Juan P.Gimenez, Mario ErnestoCaselli, Alberto TomásCiencias Exactas y NaturalesVolcanismDomuyoGeothermal FieldMicro SeismicityThermal AnomalyCiencias Exactas y NaturalesFil: Godoy, Laura. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Nacif, Silvina. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Lupari, Marianela. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: García, Héctor. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Correa-Otto, Sebastián. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Melchor, Iván. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.Fil: Pechuan, Stefanie. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Ariza, Juan. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Gimenez, Mario Ernesto. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.Fil: Caselli, Alberto. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.Cerro Domuyo, in northwestern Neuquén province of Argentina, shows notable geothermal activity, although it is located at a considerable distance from the actual volcanic arc. Many studies have been developed in this area with the aim of investigating its geothermal field. Despite these efforts, the characterization of the dynamic activity in the area is still poorly known. This work shows the results of a network of seismological stations, which registered volcano-tectonic, long-period and hybrid events. A large number of volcano-tectonic events concentrated mostly in the Cerro Domuyo geothermal area were detected. These events can be divided into two groups, those that occurred at shallow depths below the geothermal area and those at greater depths below the high region of Cerro Domuyo. Shallow events were located around the Manchana Covunco fault and many of them were particularly clustered at its intersection with the Humazo fault. Seismicity in the area shows that these faults are continually active due to fluid movement, as was evidenced by the hydrothermal manifestation of the Humazo in 2003. Moreover, new studies provide evidence that the Cerro Domuyo is experiencing an important inflation caused by a magmatic body. Deep volcano-tectonic events are evidencing this activity. Considering the large distance between the actual volcanic arc and the study region, and the high density of shallow volcano-tectonic events, it is highly likely that this magmatic body is increasing the geothermal activity. Additionally, the aeromagnetic anomaly over Cerro Domuyo is showing a thin magnetic crust of less than 6 km, suggesting a clear link between the geophysical results and the inflation in Cerro Domuyo..Elsevier2020info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfGodoy, L. B., Nacif, S., Lupari, M., García, H. P., Correa-Otto, S., Melchor, I., Pechuan, S., Ariza, J., Gimenez, M. E. & Caselli, A. T. (2021). Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuquén province, Argentina. Journal of South American Earth Sciences; 107; 102694.0895-9811https://www.sciencedirect.com/science/article/pii/S0895981120302376?via%3Dihubhttp://rid.unrn.edu.ar/handle/20.500.12049/7384https://doi.org/10.1016/j.jsames.2020.102694enghttps://www.sciencedirect.com/journal/journal-of-south-american-earth-sciences107Journal of South American Earth Sciencesinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/reponame:RID-UNRN (UNRN)instname:Universidad Nacional de Río Negro2025-09-18T10:53:03Zoai:rid.unrn.edu.ar:20.500.12049/7384instacron:UNRNInstitucionalhttps://rid.unrn.edu.ar/jspui/Universidad públicaNo correspondehttps://rid.unrn.edu.ar/oai/snrdrid@unrn.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:43692025-09-18 10:53:03.518RID-UNRN (UNRN) - Universidad Nacional de Río Negrofalse
dc.title.none.fl_str_mv Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
title Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
spellingShingle Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
Godoy, Laura B.
Ciencias Exactas y Naturales
Volcanism
Domuyo
Geothermal Field
Micro Seismicity
Thermal Anomaly
Ciencias Exactas y Naturales
title_short Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
title_full Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
title_fullStr Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
title_full_unstemmed Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
title_sort Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuqu ́en province, Argentina
dc.creator.none.fl_str_mv Godoy, Laura B.
Nacif, Silvina
Lupari, Marianela
García, Héctor P. A.
Correa-Otto, Sebastián
Melchor, Iván
Pechuan, Stefanie N.
Ariza, Juan P.
Gimenez, Mario Ernesto
Caselli, Alberto Tomás
author Godoy, Laura B.
author_facet Godoy, Laura B.
Nacif, Silvina
Lupari, Marianela
García, Héctor P. A.
Correa-Otto, Sebastián
Melchor, Iván
Pechuan, Stefanie N.
Ariza, Juan P.
Gimenez, Mario Ernesto
Caselli, Alberto Tomás
author_role author
author2 Nacif, Silvina
Lupari, Marianela
García, Héctor P. A.
Correa-Otto, Sebastián
Melchor, Iván
Pechuan, Stefanie N.
Ariza, Juan P.
Gimenez, Mario Ernesto
Caselli, Alberto Tomás
author2_role author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Ciencias Exactas y Naturales
Volcanism
Domuyo
Geothermal Field
Micro Seismicity
Thermal Anomaly
Ciencias Exactas y Naturales
topic Ciencias Exactas y Naturales
Volcanism
Domuyo
Geothermal Field
Micro Seismicity
Thermal Anomaly
Ciencias Exactas y Naturales
dc.description.none.fl_txt_mv Fil: Godoy, Laura. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Nacif, Silvina. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Lupari, Marianela. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: García, Héctor. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Correa-Otto, Sebastián. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Melchor, Iván. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.
Fil: Pechuan, Stefanie. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Ariza, Juan. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Gimenez, Mario Ernesto. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
Fil: Caselli, Alberto. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Argentina.
Cerro Domuyo, in northwestern Neuquén province of Argentina, shows notable geothermal activity, although it is located at a considerable distance from the actual volcanic arc. Many studies have been developed in this area with the aim of investigating its geothermal field. Despite these efforts, the characterization of the dynamic activity in the area is still poorly known. This work shows the results of a network of seismological stations, which registered volcano-tectonic, long-period and hybrid events. A large number of volcano-tectonic events concentrated mostly in the Cerro Domuyo geothermal area were detected. These events can be divided into two groups, those that occurred at shallow depths below the geothermal area and those at greater depths below the high region of Cerro Domuyo. Shallow events were located around the Manchana Covunco fault and many of them were particularly clustered at its intersection with the Humazo fault. Seismicity in the area shows that these faults are continually active due to fluid movement, as was evidenced by the hydrothermal manifestation of the Humazo in 2003. Moreover, new studies provide evidence that the Cerro Domuyo is experiencing an important inflation caused by a magmatic body. Deep volcano-tectonic events are evidencing this activity. Considering the large distance between the actual volcanic arc and the study region, and the high density of shallow volcano-tectonic events, it is highly likely that this magmatic body is increasing the geothermal activity. Additionally, the aeromagnetic anomaly over Cerro Domuyo is showing a thin magnetic crust of less than 6 km, suggesting a clear link between the geophysical results and the inflation in Cerro Domuyo.
.
description Fil: Godoy, Laura. CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas). Instituto Geofísico Sismológico F. Volponi, FCEFyN, Universidad Nacional de San Juan (UNSJ). Argentina.
publishDate 2020
dc.date.none.fl_str_mv 2020
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 Godoy, L. B., Nacif, S., Lupari, M., García, H. P., Correa-Otto, S., Melchor, I., Pechuan, S., Ariza, J., Gimenez, M. E. & Caselli, A. T. (2021). Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuquén province, Argentina. Journal of South American Earth Sciences; 107; 102694.
0895-9811
https://www.sciencedirect.com/science/article/pii/S0895981120302376?via%3Dihub
http://rid.unrn.edu.ar/handle/20.500.12049/7384
https://doi.org/10.1016/j.jsames.2020.102694
identifier_str_mv Godoy, L. B., Nacif, S., Lupari, M., García, H. P., Correa-Otto, S., Melchor, I., Pechuan, S., Ariza, J., Gimenez, M. E. & Caselli, A. T. (2021). Geophysical evidence of first stages of inflation in Domuyo volcanic center in northwestern Neuquén province, Argentina. Journal of South American Earth Sciences; 107; 102694.
0895-9811
url https://www.sciencedirect.com/science/article/pii/S0895981120302376?via%3Dihub
http://rid.unrn.edu.ar/handle/20.500.12049/7384
https://doi.org/10.1016/j.jsames.2020.102694
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://www.sciencedirect.com/journal/journal-of-south-american-earth-sciences
107
Journal of South American Earth Sciences
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/4.0/
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
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instname:Universidad Nacional de Río Negro
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