Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina)
- Autores
- Santos, Fernanda S.; Sommer, Carlos Augusto; Haag, Maurício Barcelos; Báez, Walter; Caselli, Alberto Tomás; Báez, Alejandro David
- Año de publicación
- 2022
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Fil: Santos, Fernanda. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil.
Fil: Sommer, Carlos. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil.
Fil: Haag, Maurício. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. Department of Earth Sciences, University of Toronto. Canada.
Fil: Báez, Walter. IBIGEO (Universidad Nacional de Salta - CONICET). Argentina.
Fil: Caselli. Alberto. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.
Fil: Báez, Alejandro. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.
Monogenetic volcanoes are among the most common volcanic landforms on Earth. The morphology and distribution of small volcanoes can provide important information about eruption dynamics and tectonics. The Southern Volcanic Zone of the Andes (CSVZ) comprises one of the most active magmatic regions on Earth. Characterized by the presence of polygenetic volcanoes and calderas in a complex tectonic setting, this region also hosts hundreds of small, back-arc monogenetic volcanoes. In this contribution, we apply a Geographic Information System (GIS) that combines imagery data and digital elevation models to establish the first comprehensive dataset of monogenetic volcanoes in the CSVZ (38◦ to 40◦ S), exploring their eruption dynamics and relationship to tectonic and structural processes. Combining spatial analysis and geomorphological observations, we identify the presence of 335 monogenetic volcanoes distributed into nine clusters, now grouped in the Zapala Volcanic Field (ZVF). The ZVF is marked by the predominance of cinder cones (80%) followed by phreatomagmatic volcanoes (20%), suggesting some influence of external water in the eruption dynamics. Generally, monogenetic vents present a clear association with local and regional lineaments, suggesting a strong structural control on the occurrence of the monogenetic deposits in the ZVF. The higher vent densities are observed in the southern Loncopu´e Though, an important extensional feature related to tearing of the subducted Nazca plate underneath the South American Plate. Morphometric parameters of cinder cones indicate variable stress orientations in the CSVZ that possibly results from the oblique tectonics in the region. From north to south, the maximum principal stress rotates from NE-SW to E-W and becomes progressively less constrained as it distances from the current magmatic arc. Based on the relative ages, we map the evolution of monogenetic volcanism through time. Our results suggest a waning in the monogenetic activity in ZVF over time. When compared to monogenetic fields in the Central Andes, the ZVF is marked by higher vent densities and number phreatomagmatic landforms, with the absence of lava domes. This ultimately reflects the contrasting crustal structure and climate conditions of these two regions.
- - Materia
-
Ciencias Exactas y Naturales
Monogenetic Volcanism
Geomorphology
Southern Volcanic Zone
Spatial Analysis
Geographic Information System
Andes
Ciencias Exactas y Naturales - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de Río Negro
- OAI Identificador
- oai:rid.unrn.edu.ar:20.500.12049/8405
Ver los metadatos del registro completo
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Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina)Santos, Fernanda S.Sommer, Carlos AugustoHaag, Maurício BarcelosBáez, WalterCaselli, Alberto TomásBáez, Alejandro DavidCiencias Exactas y NaturalesMonogenetic VolcanismGeomorphologySouthern Volcanic ZoneSpatial AnalysisGeographic Information SystemAndesCiencias Exactas y NaturalesFil: Santos, Fernanda. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil.Fil: Sommer, Carlos. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil.Fil: Haag, Maurício. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. Department of Earth Sciences, University of Toronto. Canada.Fil: Báez, Walter. IBIGEO (Universidad Nacional de Salta - CONICET). Argentina.Fil: Caselli. Alberto. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.Fil: Báez, Alejandro. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.Monogenetic volcanoes are among the most common volcanic landforms on Earth. The morphology and distribution of small volcanoes can provide important information about eruption dynamics and tectonics. The Southern Volcanic Zone of the Andes (CSVZ) comprises one of the most active magmatic regions on Earth. Characterized by the presence of polygenetic volcanoes and calderas in a complex tectonic setting, this region also hosts hundreds of small, back-arc monogenetic volcanoes. In this contribution, we apply a Geographic Information System (GIS) that combines imagery data and digital elevation models to establish the first comprehensive dataset of monogenetic volcanoes in the CSVZ (38◦ to 40◦ S), exploring their eruption dynamics and relationship to tectonic and structural processes. Combining spatial analysis and geomorphological observations, we identify the presence of 335 monogenetic volcanoes distributed into nine clusters, now grouped in the Zapala Volcanic Field (ZVF). The ZVF is marked by the predominance of cinder cones (80%) followed by phreatomagmatic volcanoes (20%), suggesting some influence of external water in the eruption dynamics. Generally, monogenetic vents present a clear association with local and regional lineaments, suggesting a strong structural control on the occurrence of the monogenetic deposits in the ZVF. The higher vent densities are observed in the southern Loncopu´e Though, an important extensional feature related to tearing of the subducted Nazca plate underneath the South American Plate. Morphometric parameters of cinder cones indicate variable stress orientations in the CSVZ that possibly results from the oblique tectonics in the region. From north to south, the maximum principal stress rotates from NE-SW to E-W and becomes progressively less constrained as it distances from the current magmatic arc. Based on the relative ages, we map the evolution of monogenetic volcanism through time. Our results suggest a waning in the monogenetic activity in ZVF over time. When compared to monogenetic fields in the Central Andes, the ZVF is marked by higher vent densities and number phreatomagmatic landforms, with the absence of lava domes. This ultimately reflects the contrasting crustal structure and climate conditions of these two regions.-El Sevier2022info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfSantos F., Sommer C., Haag M., Baez W., Caselli A., Baez A. (2022). Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina). Geomorphology; 402; 108130.0169-555Xhttps://www.sciencedirect.com/science/article/pii/S0169555X2200023X?via%3Dihub#!http://rid.unrn.edu.ar/handle/20.500.12049/8405https://doi.org/10.1016/j.geomorph.2022.108130enghttps://www.sciencedirect.com/journal/geomorphology402Geomorphologyinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/reponame:RID-UNRN (UNRN)instname:Universidad Nacional de Río Negro2025-09-29T14:29:12Zoai:rid.unrn.edu.ar:20.500.12049/8405instacron:UNRNInstitucionalhttps://rid.unrn.edu.ar/jspui/Universidad públicaNo correspondehttps://rid.unrn.edu.ar/oai/snrdrid@unrn.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:43692025-09-29 14:29:12.32RID-UNRN (UNRN) - Universidad Nacional de Río Negrofalse |
dc.title.none.fl_str_mv |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
title |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
spellingShingle |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) Santos, Fernanda S. Ciencias Exactas y Naturales Monogenetic Volcanism Geomorphology Southern Volcanic Zone Spatial Analysis Geographic Information System Andes Ciencias Exactas y Naturales |
title_short |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
title_full |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
title_fullStr |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
title_full_unstemmed |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
title_sort |
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina) |
dc.creator.none.fl_str_mv |
Santos, Fernanda S. Sommer, Carlos Augusto Haag, Maurício Barcelos Báez, Walter Caselli, Alberto Tomás Báez, Alejandro David |
author |
Santos, Fernanda S. |
author_facet |
Santos, Fernanda S. Sommer, Carlos Augusto Haag, Maurício Barcelos Báez, Walter Caselli, Alberto Tomás Báez, Alejandro David |
author_role |
author |
author2 |
Sommer, Carlos Augusto Haag, Maurício Barcelos Báez, Walter Caselli, Alberto Tomás Báez, Alejandro David |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Exactas y Naturales Monogenetic Volcanism Geomorphology Southern Volcanic Zone Spatial Analysis Geographic Information System Andes Ciencias Exactas y Naturales |
topic |
Ciencias Exactas y Naturales Monogenetic Volcanism Geomorphology Southern Volcanic Zone Spatial Analysis Geographic Information System Andes Ciencias Exactas y Naturales |
dc.description.none.fl_txt_mv |
Fil: Santos, Fernanda. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. Fil: Sommer, Carlos. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. Fil: Haag, Maurício. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. Department of Earth Sciences, University of Toronto. Canada. Fil: Báez, Walter. IBIGEO (Universidad Nacional de Salta - CONICET). Argentina. Fil: Caselli. Alberto. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina. Fil: Báez, Alejandro. Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina. Monogenetic volcanoes are among the most common volcanic landforms on Earth. The morphology and distribution of small volcanoes can provide important information about eruption dynamics and tectonics. The Southern Volcanic Zone of the Andes (CSVZ) comprises one of the most active magmatic regions on Earth. Characterized by the presence of polygenetic volcanoes and calderas in a complex tectonic setting, this region also hosts hundreds of small, back-arc monogenetic volcanoes. In this contribution, we apply a Geographic Information System (GIS) that combines imagery data and digital elevation models to establish the first comprehensive dataset of monogenetic volcanoes in the CSVZ (38◦ to 40◦ S), exploring their eruption dynamics and relationship to tectonic and structural processes. Combining spatial analysis and geomorphological observations, we identify the presence of 335 monogenetic volcanoes distributed into nine clusters, now grouped in the Zapala Volcanic Field (ZVF). The ZVF is marked by the predominance of cinder cones (80%) followed by phreatomagmatic volcanoes (20%), suggesting some influence of external water in the eruption dynamics. Generally, monogenetic vents present a clear association with local and regional lineaments, suggesting a strong structural control on the occurrence of the monogenetic deposits in the ZVF. The higher vent densities are observed in the southern Loncopu´e Though, an important extensional feature related to tearing of the subducted Nazca plate underneath the South American Plate. Morphometric parameters of cinder cones indicate variable stress orientations in the CSVZ that possibly results from the oblique tectonics in the region. From north to south, the maximum principal stress rotates from NE-SW to E-W and becomes progressively less constrained as it distances from the current magmatic arc. Based on the relative ages, we map the evolution of monogenetic volcanism through time. Our results suggest a waning in the monogenetic activity in ZVF over time. When compared to monogenetic fields in the Central Andes, the ZVF is marked by higher vent densities and number phreatomagmatic landforms, with the absence of lava domes. This ultimately reflects the contrasting crustal structure and climate conditions of these two regions. - |
description |
Fil: Santos, Fernanda. Instituto de Geociencias, Universidade Federal do Rio Grande do Sul. Brasil. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022 |
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 |
Santos F., Sommer C., Haag M., Baez W., Caselli A., Baez A. (2022). Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina). Geomorphology; 402; 108130. 0169-555X https://www.sciencedirect.com/science/article/pii/S0169555X2200023X?via%3Dihub#! http://rid.unrn.edu.ar/handle/20.500.12049/8405 https://doi.org/10.1016/j.geomorph.2022.108130 |
identifier_str_mv |
Santos F., Sommer C., Haag M., Baez W., Caselli A., Baez A. (2022). Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina). Geomorphology; 402; 108130. 0169-555X |
url |
https://www.sciencedirect.com/science/article/pii/S0169555X2200023X?via%3Dihub#! http://rid.unrn.edu.ar/handle/20.500.12049/8405 https://doi.org/10.1016/j.geomorph.2022.108130 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://www.sciencedirect.com/journal/geomorphology 402 Geomorphology |
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 |
El Sevier |
publisher.none.fl_str_mv |
El Sevier |
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reponame:RID-UNRN (UNRN) instname:Universidad Nacional de Río Negro |
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Universidad Nacional de Río Negro |
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RID-UNRN (UNRN) - Universidad Nacional de Río Negro |
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rid@unrn.edu.ar |
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