SciELO - Scientific Electronic Library Online

 
vol.60 número3Las sedimentitas que apoyan en no concordancia sobre el "granito rojo"en el angosto de la Quesera (Cordillera Oriental, Salta): una revisión crítica a más de 60 años de los trabajos pioneros de J. KeidelLa prolongación austral de las Sierras Pampeanas en la provincia de La Pampa: Evidencias geológicas y geofísicas índice de autoresíndice de assuntospesquisa de artigos
Home Pagelista alfabética de periódicos  

Serviços Personalizados

Journal

Artigo

Indicadores

  • Não possue artigos citadosCitado por SciELO

Links relacionados

  • Não possue artigos similaresSimilares em SciELO

Compartilhar


Revista de la Asociación Geológica Argentina

versão impressa ISSN 0004-4822versão On-line ISSN 1851-8249

Resumo

GIAMBIAGI, L.B.; SURIANO, J.  e  MAESCUA, J.. Multiepisodic extension during the Early Jurassic in the Atuel depocentre of the Neuquén basin. Rev. Asoc. Geol. Argent. [online]. 2005, vol.60, n.3, pp.524-534. ISSN 0004-4822.

Structural and paleostress studies of the northernmost part of the Atuel depocentre of the Neuquén basin show that the area has undergone at least two rifting episodes during the Lower Jurassic. The first episode occurred during the deposition of the El Freno fluvial strata, with the development of a series of NNE trending faults. It is likely that the NE to NNE inherited structural lineations of the Paleozoic basement had a strong control during this extensional stage. As the ENE extensional direction was oblique to these pre-existing structures, there was a sinistral strike-slip movement along the rift faults. The second rifting event developed during the deposition of the lower part of the Puesto Araya Formation marine sediments and its faults were localized close to the main rift normal fault, which has a NNW trend.

Palavras-chave : Neuquén basin; Atuel depocenter; Multiepisodic extension; Oblique extension; Paleostress.

        · resumo em Espanhol     · texto em Espanhol     · Espanhol ( pdf )

 

Creative Commons License Todo o conteúdo deste periódico, exceto onde está identificado, está licenciado sob uma Licença Creative Commons