Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile

Autores
Niemeyer, Hans; Zavattieri, Ana María; Ballent, Sara Cristina; Zamuner, Alba Berta; Gallego, Oscar Florencio
Año de publicación
2008
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almelda, Antofagasta) that in previous papers was attributed to either the Late Paleozoic or Triassic. At Quebrada del Medio, the Pular Formation includes a 379-meter-thick stratigraphic section formed from base to top by conglomerates, sandstones, black bituminous shales and limestones, tuffaceous sandstones and a poorly welded ignimbrite that , accumulated in fluvial and lacustrine environments. A multidisciplinary study of the flora and fauna was undertaken. The existence of diagnostic Gondwana microflora and macroflora allows attributing a Middle Triassic to early Late Triassic age to the Pular Formation.
Facultad de Ciencias Naturales y Museo
Materia
Geología
Chile
Fluvial and lacustrine environments
Gondwana flora
Pular Formation
Triassic
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/82958
Acceder
id SEDICI_ce848e84a7ef2886aa7c1f811f3edc4c
oai_identifier_str oai:sedici.unlp.edu.ar:10915/82958
network_acronym_str SEDICI
repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern ChileNiemeyer, HansZavattieri, Ana MaríaBallent, Sara CristinaZamuner, Alba BertaGallego, Oscar FlorencioGeologíaChileFluvial and lacustrine environmentsGondwana floraPular FormationTriassicIn this contribution, we present a reassessment of the Pular Formation age (Sierra de Almelda, Antofagasta) that in previous papers was attributed to either the Late Paleozoic or Triassic. At Quebrada del Medio, the Pular Formation includes a 379-meter-thick stratigraphic section formed from base to top by conglomerates, sandstones, black bituminous shales and limestones, tuffaceous sandstones and a poorly welded ignimbrite that , accumulated in fluvial and lacustrine environments. A multidisciplinary study of the flora and fauna was undertaken. The existence of diagnostic Gondwana microflora and macroflora allows attributing a Middle Triassic to early Late Triassic age to the Pular Formation.Facultad de Ciencias Naturales y Museo2008info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf147-161http://sedici.unlp.edu.ar/handle/10915/82958enginfo:eu-repo/semantics/altIdentifier/issn/0716-0208info:eu-repo/semantics/altIdentifier/doi/10.4067/S0716-02082008000100007info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc/4.0/Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:15:41Zoai:sedici.unlp.edu.ar:10915/82958Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:15:41.985SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
title Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
spellingShingle Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
Niemeyer, Hans
Geología
Chile
Fluvial and lacustrine environments
Gondwana flora
Pular Formation
Triassic
title_short Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
title_full Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
title_fullStr Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
title_full_unstemmed Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
title_sort Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
dc.creator.none.fl_str_mv Niemeyer, Hans
Zavattieri, Ana María
Ballent, Sara Cristina
Zamuner, Alba Berta
Gallego, Oscar Florencio
author Niemeyer, Hans
author_facet Niemeyer, Hans
Zavattieri, Ana María
Ballent, Sara Cristina
Zamuner, Alba Berta
Gallego, Oscar Florencio
author_role author
author2 Zavattieri, Ana María
Ballent, Sara Cristina
Zamuner, Alba Berta
Gallego, Oscar Florencio
author2_role author
author
author
author
dc.subject.none.fl_str_mv Geología
Chile
Fluvial and lacustrine environments
Gondwana flora
Pular Formation
Triassic
topic Geología
Chile
Fluvial and lacustrine environments
Gondwana flora
Pular Formation
Triassic
dc.description.none.fl_txt_mv In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almelda, Antofagasta) that in previous papers was attributed to either the Late Paleozoic or Triassic. At Quebrada del Medio, the Pular Formation includes a 379-meter-thick stratigraphic section formed from base to top by conglomerates, sandstones, black bituminous shales and limestones, tuffaceous sandstones and a poorly welded ignimbrite that , accumulated in fluvial and lacustrine environments. A multidisciplinary study of the flora and fauna was undertaken. The existence of diagnostic Gondwana microflora and macroflora allows attributing a Middle Triassic to early Late Triassic age to the Pular Formation.
Facultad de Ciencias Naturales y Museo
description In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almelda, Antofagasta) that in previous papers was attributed to either the Late Paleozoic or Triassic. At Quebrada del Medio, the Pular Formation includes a 379-meter-thick stratigraphic section formed from base to top by conglomerates, sandstones, black bituminous shales and limestones, tuffaceous sandstones and a poorly welded ignimbrite that , accumulated in fluvial and lacustrine environments. A multidisciplinary study of the flora and fauna was undertaken. The existence of diagnostic Gondwana microflora and macroflora allows attributing a Middle Triassic to early Late Triassic age to the Pular Formation.
publishDate 2008
dc.date.none.fl_str_mv 2008
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Articulo
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://sedici.unlp.edu.ar/handle/10915/82958
url http://sedici.unlp.edu.ar/handle/10915/82958
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/issn/0716-0208
info:eu-repo/semantics/altIdentifier/doi/10.4067/S0716-02082008000100007
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc/4.0/
Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc/4.0/
Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
dc.format.none.fl_str_mv application/pdf
147-161
dc.source.none.fl_str_mv reponame:SEDICI (UNLP)
instname:Universidad Nacional de La Plata
instacron:UNLP
reponame_str SEDICI (UNLP)
collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
instacron_str UNLP
institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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score 13.070432

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