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(Article of periodic en Anglais - 2009)

Document title

Morphodynamics and seismostratigraphy of a deep hole at tidal channel confluence

Authors(s) and Affiliation(s)

GINSBERG S.S. (1 2) ; ALIOTTA S. (1 3) ; LIZASOAIN G.O. (1) ;
(1) Inst. Argentino de Oceanografía, CCT-CONICET-BB, Bahía Blanca, ARGENTINE
(2) Univ. Tecnológica Nacional, FRBB, Dpto Ingeniería Civil, Bahía Blanca, ARGENTINE
(3) Univ. Nacional del Sur, Dpto. Geología, Bahía Blanca, ARGENTINE

Abstract

This paper describes the dominant bed load transport circulatory pattern over the tidal channel confluence as well as the scour hole genesis and evolution in Bahía Blanca estuary, Argentina. In addition, the AA. detail the bed morphology associated with the sediment availability of each channel and sedimentary facies. As scour holes exhibit similar characteristics, their focus of attention was centred on a scour hole located inward, in the first bifurcation of Tres Brazas channel. The seismostratigraphic information collected in this study indicates that the depression was originally a fully erosive morphological feature. A descriptive model of the morphological evolution at a channel confluence is presented in this study

Source

Article of periodic

published at : Geomorphology / ISSN 0169-555X

Editor : Elsevier, Amsterdam - PAYS-BAS (1987)

Millesime : 2009, vol. 104, no3-4 [pp. 253-261]

Bibliographic references : 1 p.

Collation : 6 fig.

Language

Anglais

INIST-CNRS, Cote INIST : 21151

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1016/j.geomorph.2008.09.002

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2010
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