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

In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almeida, 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...

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Autores principales: Niemeyer,Hans, Zavattieri,Ana María, Ballent,Sara, Zamuner,Alba, Gallego,Oscar
Lenguaje:English
Publicado: Servicio Nacional de Geología y Minería (SERNAGEOMIN) 2008
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082008000100007
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spelling oai:scielo:S0716-020820080001000072008-04-10Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern ChileNiemeyer,HansZavattieri,Ana MaríaBallent,SaraZamuner,AlbaGallego,Oscar Pular Formation Triassic Gondwana flora Fluvial and lacustrine environments Chile In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almeida, 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 Formationinfo:eu-repo/semantics/openAccessServicio Nacional de Geología y Minería (SERNAGEOMIN)Revista geológica de Chile v.35 n.1 20082008-01-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082008000100007en10.4067/S0716-02082008000100007
institution Scielo Chile
collection Scielo Chile
language English
topic Pular Formation
Triassic
Gondwana flora
Fluvial and lacustrine environments
Chile
spellingShingle Pular Formation
Triassic
Gondwana flora
Fluvial and lacustrine environments
Chile
Niemeyer,Hans
Zavattieri,Ana María
Ballent,Sara
Zamuner,Alba
Gallego,Oscar
Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
description In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almeida, 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
author Niemeyer,Hans
Zavattieri,Ana María
Ballent,Sara
Zamuner,Alba
Gallego,Oscar
author_facet Niemeyer,Hans
Zavattieri,Ana María
Ballent,Sara
Zamuner,Alba
Gallego,Oscar
author_sort Niemeyer,Hans
title Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile
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
publisher Servicio Nacional de Geología y Minería (SERNAGEOMIN)
publishDate 2008
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082008000100007
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