Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)

The seaward end of modern rivers is characterized by the interactions of marine and fluvial processes, a tract known as the fluvial to marine transition zone, which varies between systems due to the relative strength of these processes. To understand how fluvial and tidal process interactions and th...

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Detalles Bibliográficos
Autores principales: Gugliotta, Marcello, Flint, Stephen S., Hodgson, David M., Veiga, Gonzalo Diego
Formato: Articulo Preprint
Lenguaje:Inglés
Publicado: 2016
Materias:
Geología
Fluvial-dominated
Tide-influenced
Backwater
Microtidal
Jurassic
Neuquén Basin
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/128498
Aporte de:
SEDICI (UNLP) de Universidad Nacional de La Plata
id I19-R120-10915-128498
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Geología
Fluvial-dominated
Tide-influenced
Backwater
Microtidal
Jurassic
Neuquén Basin
spellingShingle Geología
Fluvial-dominated
Tide-influenced
Backwater
Microtidal
Jurassic
Neuquén Basin
Gugliotta, Marcello
Flint, Stephen S.
Hodgson, David M.
Veiga, Gonzalo Diego
Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
topic_facet Geología
Fluvial-dominated
Tide-influenced
Backwater
Microtidal
Jurassic
Neuquén Basin
description The seaward end of modern rivers is characterized by the interactions of marine and fluvial processes, a tract known as the fluvial to marine transition zone, which varies between systems due to the relative strength of these processes. To understand how fluvial and tidal process interactions and the fluvial to marine transition zone are preserved in the rock record, large-scale outcrops of deltaic deposits of the Middle Jurassic Lajas Formation (Neuquen Basin, Argentina) have been investigated. Fluvial–tidal indicators consist of cyclically distributed carbonaceous drapes in unidirectional, seaward-oriented cross-stratifications, which are interpreted as the result of tidal modulation of the fluvial current in the inner part of the fluvial to marine transition zone. Heterolithic deposits with decimetre-scale interbedding of coarser-grained and finer-grained facies with mixed fluvial and tidal affinities are interpreted to indicate fluvial discharge fluctuations (seasonality) and subordinate tidal influence. Many other potential tidal indicators are argued to be the result of fluvial–tidal interactions with overall fluvial dominance or of purely fluvial processes. No purely tidal or tide-dominated facies were recognized in the studied deposits. Moreover, fluvial–tidal features are found mainly in deposits interpreted as interflood (forming during low river stage) in distal (delta front) or off-axis (interdistributary) parts of the system. Along major channel axes, the interpreted fluvial to marine transition zone is mainly represented by the fluvial-dominated section, whereas little or no tide-dominated section is identified. The system is interpreted to have been hyposynchronous with a poorly developed turbidity maximum. These conditions and the architectural elements described, including major and minor distributary channels, terminal distributary channels, mouth bars and crevasse mouth bars, are consistent with an interpretation of a fluvial-dominated, tide-influenced delta system and with an estimated short backwater length and inferred microtidal conditions. The improved identification of process interactions, and their preservation in ancient fluvial to marine transition zones, is fundamental to refining interpretations of ancient deltaic successions.
format Articulo
Preprint
author Gugliotta, Marcello
Flint, Stephen S.
Hodgson, David M.
Veiga, Gonzalo Diego
author_facet Gugliotta, Marcello
Flint, Stephen S.
Hodgson, David M.
Veiga, Gonzalo Diego
author_sort Gugliotta, Marcello
title Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
title_short Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
title_full Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
title_fullStr Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
title_full_unstemmed Recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (Lajas Formation, Argentina)
title_sort recognition criteria, characteristics and implications of the fluvial to marine transition zone in ancient deltaic deposits (lajas formation, argentina)
publishDate 2016
url http://sedici.unlp.edu.ar/handle/10915/128498
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