Artículo

La versión final de este artículo es de uso interno. El editor solo permite incluir en el repositorio el artículo en su versión post-print. Por favor, si usted la posee enviela a
Consulte el artículo en la página del editor
Consulte la política de Acceso Abierto del editor

Abstract:

Late Paleozoic glacial diamictites occur in many localities in western Argentina, indicating that the region was strongly affected by glaciation during the mid-Carboniferous (late Serpukhovian-early Bashkirian). In most instances these diamictites are found in steeply walled paleovalley settings in the Andean Precordillera. This study presents new data from a locality north of the Precordillera that suggests an additional, distinct, volume of ice existed in the region during the Carboniferous. The glacigenic diamictites in the Rio Blanco Basin were ultimately emplaced as gravity flows, precluding inferences of paleo-ice volume. Fold nose orientation and soft-sediment groove orientations within the diamictites indicate that the deposits were emplaced from north to south, suggesting that glacial ice was most likely not sourced from the proto-Precordillera at this locality, requiring the need for another ice center to the north of the basin. Diamictite facies indicates that the sediment was initially supplied to the study area by a warm-based glacier. © 2013 International Association for Gondwana Research.

Registro:

Documento: Artículo
Título:Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
Autor:Gulbranson, E.L.; Isbell, J.L.; Montañez, I.P.; Limarino, C.O.; Marenssi, S.A.; Meyer, K.; Hull, C.
Filiación:Department of Geology, University of California-Davis, One Shields Ave, Davis, CA 95616, USA
Department of Geosciences, University of Wisconsin-Milwaukee, Milwaukee, WI 53211, USA
Department of Geology, University of Buenos Aires, Cuidad Universitaria, Pabellón II, 1428, Buenos Aires, Argentina
Consejo Nacional de Investigaciones Cientificas y Técnicas (CONICET), Argentina
Instituto Antártico Argentino, Cerrito 1248, C1010AAZ, Buenos Aires, Argentina
Idioma: Inglés
Palabras clave:Carboniferous; Diamictite; Gondwana; Late Paleozoic ice age; Mass transport
Año:2013
DOI: http://dx.doi.org/10.1016/j.gr.2013.03.017
Título revista:Gondwana Research
Título revista abreviado:Gondwana Res.
ISSN:1342937X
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1342937X_v_n_p_Gulbranson

Citas:

---------- APA ----------
Gulbranson, E.L., Isbell, J.L., Montañez, I.P., Limarino, C.O., Marenssi, S.A., Meyer, K. & Hull, C. (2013) . Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites. Gondwana Research.
http://dx.doi.org/10.1016/j.gr.2013.03.017
---------- CHICAGO ----------
Gulbranson, E.L., Isbell, J.L., Montañez, I.P., Limarino, C.O., Marenssi, S.A., Meyer, K., et al. "Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites" . Gondwana Research (2013).
http://dx.doi.org/10.1016/j.gr.2013.03.017
---------- MLA ----------
Gulbranson, E.L., Isbell, J.L., Montañez, I.P., Limarino, C.O., Marenssi, S.A., Meyer, K., et al. "Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites" . Gondwana Research, 2013.
http://dx.doi.org/10.1016/j.gr.2013.03.017
---------- VANCOUVER ----------
Gulbranson, E.L., Isbell, J.L., Montañez, I.P., Limarino, C.O., Marenssi, S.A., Meyer, K., et al. Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites. Gondwana Res. 2013.
http://dx.doi.org/10.1016/j.gr.2013.03.017