Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina

Autores
Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Arnous, Ahmad
Año de publicación
2022
Idioma
inglés
Tipo de recurso
parte de libro
Estado
versión publicada
Descripción
Structural geoforms often allow us to interpret the processes that gave rise to them. Circular geoforms are normally associated with meteorite falls, with the volcano caldera or the intrusion of igneous bodies, and elliptical geoforms with tectonic processes. We describe eight circular morphological features representing depressed areas based on visual interpretations from satellite and radar scans images. Three geoforms are located at the northern of the Sierras Pampeanas and the others five in Chacopampeana plain in Argentina. The La Ciénaga circular structure is 15 km in diameter, Las Cejas is 34 km in diameter and Schaqui is 21 km in diameter. The semicircular structures of the Chacopampeana plain (Las Víboras, El Fadeté, La Irma and Laguna de los Cisnes) are between 15 and 31.5 km in diameter. The elongated Campo del Cielo structure connected to the El Fadeté structure has an E-W strike, 12 km long and 4km wide, similar characteristics to those described in the literature. These studied structures have no associated volcanic rocks and no evidence of tectonic activity is observed. The La Ciénaga structure is a depression covered by quaternary sediments. The Schaqui structure is formed in an environment of intrusive rocks and its morphology is marked by the contact between them. In the Las Cejas structure, seismic profiles show the normal fault of one of its edges and the basin generated in its center. In Campo del Cielo several structures were found associated with the fall of meteorites; the structures described there seem to be formed by the impact of an object and contrast with the monotony of the rest of the area. Until now rings of these characteristics, magnitudes and diameters are unknown and unheard of in Argentina.
Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; Argentina
Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Arnous, Ahmad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Materia
Impact structures
Meteorites
Geoforms
Pampean ranges
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/225464

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spelling Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, ArgentinaGutierrez, Adolfo AntonioMon, RicardoCisterna, Clara EugeniaArnous, AhmadImpact structuresMeteoritesGeoformsPampean rangeshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Structural geoforms often allow us to interpret the processes that gave rise to them. Circular geoforms are normally associated with meteorite falls, with the volcano caldera or the intrusion of igneous bodies, and elliptical geoforms with tectonic processes. We describe eight circular morphological features representing depressed areas based on visual interpretations from satellite and radar scans images. Three geoforms are located at the northern of the Sierras Pampeanas and the others five in Chacopampeana plain in Argentina. The La Ciénaga circular structure is 15 km in diameter, Las Cejas is 34 km in diameter and Schaqui is 21 km in diameter. The semicircular structures of the Chacopampeana plain (Las Víboras, El Fadeté, La Irma and Laguna de los Cisnes) are between 15 and 31.5 km in diameter. The elongated Campo del Cielo structure connected to the El Fadeté structure has an E-W strike, 12 km long and 4km wide, similar characteristics to those described in the literature. These studied structures have no associated volcanic rocks and no evidence of tectonic activity is observed. The La Ciénaga structure is a depression covered by quaternary sediments. The Schaqui structure is formed in an environment of intrusive rocks and its morphology is marked by the contact between them. In the Las Cejas structure, seismic profiles show the normal fault of one of its edges and the basin generated in its center. In Campo del Cielo several structures were found associated with the fall of meteorites; the structures described there seem to be formed by the impact of an object and contrast with the monotony of the rest of the area. Until now rings of these characteristics, magnitudes and diameters are unknown and unheard of in Argentina.Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; ArgentinaFil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaFil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaFil: Arnous, Ahmad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaBook Publisher InternationalYu, Huan2022info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/bookParthttp://purl.org/coar/resource_type/c_3248info:ar-repo/semantics/parteDeLibroapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/225464Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Arnous, Ahmad; Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina; Book Publisher International; 5; 2022; 120-143978-93-90431-12-0CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://bp.bookpi.org/index.php/bpi/catalog/book/279info:eu-repo/semantics/altIdentifier/url/http://dx.doi.org/10.9734/bpi/ireges/v5info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:42:57Zoai:ri.conicet.gov.ar:11336/225464instacron: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 10:42:57.585CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
title Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
spellingShingle Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
Gutierrez, Adolfo Antonio
Impact structures
Meteorites
Geoforms
Pampean ranges
title_short Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
title_full Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
title_fullStr Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
title_full_unstemmed Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
title_sort Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina
dc.creator.none.fl_str_mv Gutierrez, Adolfo Antonio
Mon, Ricardo
Cisterna, Clara Eugenia
Arnous, Ahmad
author Gutierrez, Adolfo Antonio
author_facet Gutierrez, Adolfo Antonio
Mon, Ricardo
Cisterna, Clara Eugenia
Arnous, Ahmad
author_role author
author2 Mon, Ricardo
Cisterna, Clara Eugenia
Arnous, Ahmad
author2_role author
author
author
dc.contributor.none.fl_str_mv Yu, Huan
dc.subject.none.fl_str_mv Impact structures
Meteorites
Geoforms
Pampean ranges
topic Impact structures
Meteorites
Geoforms
Pampean ranges
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Structural geoforms often allow us to interpret the processes that gave rise to them. Circular geoforms are normally associated with meteorite falls, with the volcano caldera or the intrusion of igneous bodies, and elliptical geoforms with tectonic processes. We describe eight circular morphological features representing depressed areas based on visual interpretations from satellite and radar scans images. Three geoforms are located at the northern of the Sierras Pampeanas and the others five in Chacopampeana plain in Argentina. The La Ciénaga circular structure is 15 km in diameter, Las Cejas is 34 km in diameter and Schaqui is 21 km in diameter. The semicircular structures of the Chacopampeana plain (Las Víboras, El Fadeté, La Irma and Laguna de los Cisnes) are between 15 and 31.5 km in diameter. The elongated Campo del Cielo structure connected to the El Fadeté structure has an E-W strike, 12 km long and 4km wide, similar characteristics to those described in the literature. These studied structures have no associated volcanic rocks and no evidence of tectonic activity is observed. The La Ciénaga structure is a depression covered by quaternary sediments. The Schaqui structure is formed in an environment of intrusive rocks and its morphology is marked by the contact between them. In the Las Cejas structure, seismic profiles show the normal fault of one of its edges and the basin generated in its center. In Campo del Cielo several structures were found associated with the fall of meteorites; the structures described there seem to be formed by the impact of an object and contrast with the monotony of the rest of the area. Until now rings of these characteristics, magnitudes and diameters are unknown and unheard of in Argentina.
Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; Argentina
Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Arnous, Ahmad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
description Structural geoforms often allow us to interpret the processes that gave rise to them. Circular geoforms are normally associated with meteorite falls, with the volcano caldera or the intrusion of igneous bodies, and elliptical geoforms with tectonic processes. We describe eight circular morphological features representing depressed areas based on visual interpretations from satellite and radar scans images. Three geoforms are located at the northern of the Sierras Pampeanas and the others five in Chacopampeana plain in Argentina. The La Ciénaga circular structure is 15 km in diameter, Las Cejas is 34 km in diameter and Schaqui is 21 km in diameter. The semicircular structures of the Chacopampeana plain (Las Víboras, El Fadeté, La Irma and Laguna de los Cisnes) are between 15 and 31.5 km in diameter. The elongated Campo del Cielo structure connected to the El Fadeté structure has an E-W strike, 12 km long and 4km wide, similar characteristics to those described in the literature. These studied structures have no associated volcanic rocks and no evidence of tectonic activity is observed. The La Ciénaga structure is a depression covered by quaternary sediments. The Schaqui structure is formed in an environment of intrusive rocks and its morphology is marked by the contact between them. In the Las Cejas structure, seismic profiles show the normal fault of one of its edges and the basin generated in its center. In Campo del Cielo several structures were found associated with the fall of meteorites; the structures described there seem to be formed by the impact of an object and contrast with the monotony of the rest of the area. Until now rings of these characteristics, magnitudes and diameters are unknown and unheard of in Argentina.
publishDate 2022
dc.date.none.fl_str_mv 2022
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/bookPart
http://purl.org/coar/resource_type/c_3248
info:ar-repo/semantics/parteDeLibro
status_str publishedVersion
format bookPart
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/225464
Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Arnous, Ahmad; Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina; Book Publisher International; 5; 2022; 120-143
978-93-90431-12-0
CONICET Digital
CONICET
url http://hdl.handle.net/11336/225464
identifier_str_mv Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Arnous, Ahmad; Circular Natural Geoforms, Sierras Pampeanas and Chacopampeana Plain, Argentina; Book Publisher International; 5; 2022; 120-143
978-93-90431-12-0
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://bp.bookpi.org/index.php/bpi/catalog/book/279
info:eu-repo/semantics/altIdentifier/url/http://dx.doi.org/10.9734/bpi/ireges/v5
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
application/pdf
dc.publisher.none.fl_str_mv Book Publisher International
publisher.none.fl_str_mv Book Publisher International
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
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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
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