Review of the Cambrian Stratigraphy of the Argentine Precordillera

Autor: Bordonaro, Osvaldo Luís
Jazyk: angličtina
Rok vydání: 2003
Předmět:
Zdroj: Geologica Acta; Vol. 1 No 1 (2003); 11-22
Geologica Acta; Vol. 1 No. 1 (2003): Advances in the knowledge of the Cambrian System; 11-22
Geologica Acta; Vol. 1 Núm. 1 (2003); 11-22
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
RCUB. Revistas Científicas de la Universidad de Barcelona
instname
Recercat. Dipósit de la Recerca de Catalunya
Geologica Acta; 2003: Vol.: 1 Núm.: 1; p. 11
ISSN: 1695-6133
1696-5728
Popis: The Cambrian rocks of the Argentine Precordillera are analyzed and updated providing a new stratigraphic interpretation. The lithostratigraphic assemblages provide evidence that the Precordilleran Cambrian Basin was a rimmed platform. The lithostratigraphy record enables to distinguish three large areas corresponding to an inner platform, an outer platform to slope environment and a mixed zone where both platforms and the rim interfinger. The biostratigraphic proposal based on trilobites include restricted shelf biozones to the East, characterized by sparse, endemic and low diversity polymeroid faunules. Moreover, to the West outer shelf biozones are characterized by widespread, high diversity, mixed endemic and cosmopolitan polymeroid and agnostoid faunas. The lithostratigraphic and biostratigraphic data prove the existence of an important hiatus near the Lower-Middle Cambrian boundary, which is correlated to the Hawke Bay regressive event recorded along the eastern margin of Laurentia. The Olenellus Zone assemblage trilobites underlies the Glossopleura or the Ehmaniella Zone. The early Middle Cambrian zones (from Plagiura-Poliella to Albertella) are lacking in the whole Precordillera.
Databáze: OpenAIRE
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