The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)

The San Ignacio Fm, a late Palaeozoic foreland basin succession that crops out in the Frontal Cordillera (Argentinean Andes), contains lacustrine microbial carbonates and volcanic rocks. Modification by extensive pedogenic processes contributed to the massive aspect of the calcareous beds. Most of t...

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Autores: Busquest, P., Méndez Bedia, Isabel, Gallastegui, Gloria, Colombo, F., Cardó, R., Limarino, Carlos Oscar, Heredia, N., Cesari, Silvia Nelida
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2013
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:inglés
OAI Identifier:oai:ri.conicet.gov.ar:11336/8611
Acceso en línea:http://hdl.handle.net/11336/8611
Access Level:acceso abierto
Palabra clave:Microbial Carbonates
Volcanic
Palaeosols
Late Palaeozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
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spelling The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)Busquest, P.Méndez Bedia, IsabelGallastegui, GloriaColombo, F.Cardó, R.Limarino, Carlos OscarHeredia, N.Cesari, Silvia NelidaMicrobial CarbonatesVolcanicPalaeosolsLate Palaeozoichttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The San Ignacio Fm, a late Palaeozoic foreland basin succession that crops out in the Frontal Cordillera (Argentinean Andes), contains lacustrine microbial carbonates and volcanic rocks. Modification by extensive pedogenic processes contributed to the massive aspect of the calcareous beds. Most of the volcanic deposits in the San Ignacio Fm consist of pyroclastic rocks and resedimented volcaniclastic deposits. Less frequent lava flows produced during effusive eruptions led to the generation of tabular layers of fine-grained, greenish or grey andesites, trachytes and dacites. Pyroclastic flow deposits correspond mainly to welded ignimbrites made up of former glassy pyroclasts devitrified to microcrystalline groundmass, scarce crystals of euhedral plagioclase, quartz and K-feldspar, opaque minerals, aggregates of fine-grained phyllosilicates and fiammes defining a bedding-parallel foliation generated by welding or diagenetic compaction.Fil: Busquest, P.. Universidad de Barcelona; EspañaFil: Méndez Bedia, Isabel. Universidad de Oviedo; EspañaFil: Gallastegui, Gloria. Instituto Geológico y Minero de España; EspañaFil: Colombo, F.. Universidad de Barcelona; EspañaFil: Cardó, R.. Secretaría de Industria y Minería. Servicio Geologico Minero Argentino; ArgentinaFil: Limarino, Carlos Oscar. Universidad de Buenos Aires. Departamento de Ciencias Exactas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Heredia, N.. Instituto Geológico y Minero de España; EspañaFil: Cesari, Silvia Nelida. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales; ArgentinaSpringer2013-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/8611Busquest, P.; Méndez Bedia, Isabel; Gallastegui, Gloria; Colombo, F.; Cardó, R.; et al.; The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina); Springer; International Journal Of Earth Sciences; 102; 5; 1-3-2013; 1271-12871437-3254enginfo:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-013-0870-zinfo:eu-repo/semantics/altIdentifier/url/http://link.springer.com/article/10.1007/s00531-013-0870-zinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2024-05-08T14:25:44Zoai:ri.conicet.gov.ar:11336/8611instacron: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:34982024-05-08 14:25:44.397CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
title The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
spellingShingle The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
Busquest, P.
Microbial Carbonates
Volcanic
Palaeosols
Late Palaeozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
title_short The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
title_full The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
title_fullStr The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
title_full_unstemmed The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
title_sort The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina)
dc.creator.none.fl_str_mv Busquest, P.
Méndez Bedia, Isabel
Gallastegui, Gloria
Colombo, F.
Cardó, R.
Limarino, Carlos Oscar
Heredia, N.
Cesari, Silvia Nelida
author Busquest, P.
author_facet Busquest, P.
Méndez Bedia, Isabel
Gallastegui, Gloria
Colombo, F.
Cardó, R.
Limarino, Carlos Oscar
Heredia, N.
Cesari, Silvia Nelida
author_role author
author2 Méndez Bedia, Isabel
Gallastegui, Gloria
Colombo, F.
Cardó, R.
Limarino, Carlos Oscar
Heredia, N.
Cesari, Silvia Nelida
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Microbial Carbonates
Volcanic
Palaeosols
Late Palaeozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic Microbial Carbonates
Volcanic
Palaeosols
Late Palaeozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description The San Ignacio Fm, a late Palaeozoic foreland basin succession that crops out in the Frontal Cordillera (Argentinean Andes), contains lacustrine microbial carbonates and volcanic rocks. Modification by extensive pedogenic processes contributed to the massive aspect of the calcareous beds. Most of the volcanic deposits in the San Ignacio Fm consist of pyroclastic rocks and resedimented volcaniclastic deposits. Less frequent lava flows produced during effusive eruptions led to the generation of tabular layers of fine-grained, greenish or grey andesites, trachytes and dacites. Pyroclastic flow deposits correspond mainly to welded ignimbrites made up of former glassy pyroclasts devitrified to microcrystalline groundmass, scarce crystals of euhedral plagioclase, quartz and K-feldspar, opaque minerals, aggregates of fine-grained phyllosilicates and fiammes defining a bedding-parallel foliation generated by welding or diagenetic compaction.
publishDate 2013
dc.date.none.fl_str_mv 2013-03-01
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/11336/8611
Busquest, P.; Méndez Bedia, Isabel; Gallastegui, Gloria; Colombo, F.; Cardó, R.; et al.; The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina); Springer; International Journal Of Earth Sciences; 102; 5; 1-3-2013; 1271-1287
1437-3254
url http://hdl.handle.net/11336/8611
identifier_str_mv Busquest, P.; Méndez Bedia, Isabel; Gallastegui, Gloria; Colombo, F.; Cardó, R.; et al.; The relationship between carbonate facies, volcanic rocks and plant remains in a late Palaeozoic lacustrine system (San Ignacio Fm, Frontal Cordillera, San Juan province, Argentina); Springer; International Journal Of Earth Sciences; 102; 5; 1-3-2013; 1271-1287
1437-3254
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-013-0870-z
info:eu-repo/semantics/altIdentifier/url/http://link.springer.com/article/10.1007/s00531-013-0870-z
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 Springer
publisher.none.fl_str_mv Springer
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
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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