Controles sobre la interacción fluvial-lacustre en un rift triásico del oeste argentino
- Autores: Luis A. Spalletti
- Localización: Geotemas (Madrid), ISSN 1576-5172, Nº. 3, 2, 2001 (Ejemplar dedicado a: XIV Congreso Nacional de Sedimentología, IV Congreso del Cretácico de España), págs. 99-102
- Idioma: español
- Enlaces
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Resumen
Siliciclastic facies and depositional systems are studied in the Triassic outcrops located along the western margin of the Precordillera (San Juan Province). In the Hilario region the Triassic section begins with pyroclastic flow- and fall-deposits associated with fluvial (volcaniclastic) deposits.
The middle and upper sections of the El Alcázar Fm. are dominated by lacustrine sediments. In the Barreal region the record begins with braided deposits (lower to middle Barreal Fm.) and is followed by a lacustrine system (upper Barreal and lower Cortaderita Fms.). A significant palaeogeographic change produced the substitution o f the lacustrine system by a sandy-braided system and a tuffaceous plain (upper Cortaderita Fm.). The Triassic record ends with the alluvial and ephemeral fluvial red beds of the Cepeda Fm.
The studied deposits represent the infill of the passive flank or ramp of a Triassic half-graben. Three depositional sequences were defined. DS 1 starts with braided river deposits associated with pyroclastic flow- and fall-deposits, and ends with holomictic and meromictic lacustrine systems showing several episodes of deltaic progradation. DS 2 develops on a marked regional unconformity and is composed of sandy-braided deposits followed by tuffaceous facies (aeolian and high-sinuosity fluvial deposits). Proximal fluvial deposits (alluvial and ephemeral systems), resulting from a regional tectonic reactivation and a climatic change towards more arid conditions, are the main building units of DS 3.
Tractional fluvial facies represent degradational systems tracts, mixed-load fluvial facies associations are the main depositional units of transitional systems tracts, and lacustrine deposits are the record of aggradational systems tracts. These deposits do not show a clear megasequence stacking because of the interaction o f multiple allocyclic controls, such as local tectonism, base level oscillations, variations in base profile, variations in coarse-grained contribution, and coeval explosive volcan ism.
Definition of depositional sequences bounded by regional unconformities resulted an important tool for stratigraphic correlation. However, gravelly and sandy sediment-bodies intercalated within lacustrine successions must be avoided for correlation since they represent autocydic progradations of deltaic lobes.
