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Abstract:

Namurian-early Westphalian glacial-postglacial deposits have been documented in the Paganzo Basin, Argentina, but integrated sequence stratigraphic and sedimentological analyses of the glacial-postglacial transition are rare. In the Cuesta de Huaco section the glacial-postglacial transition encompasses the lower sequence of the existing schemes. Glacioeustatic changes in sea-level controlled the architecture and vertical arrangement of fades. The basal sequence boundary is coeval with the onset of glaciation when sea level fell, contemporaneous with glacial erosion and bypass of sediment. The upper sequence boundary is a high-frequency sequence boundary. The basal deposits are interpreted as an early transgressive systems tract (ETST) initiated during glacial retreat. The interval fines upward, contains current reworked diamictites, conglomerates and sandstones deposited in a subglacial to proglacial environment (Facies I-II) and ice-rafted glaciomarine rhythmites (Facies III). Postglacial brackish-marine black shales (Facies IV) represent the late transgressive systems tract (LTST). Micritic-limestone beds were deposited during a period of sediment starvation coeval with the maximum marine inundation in the basin (MFZ). It marks a turnaround in the stacking pattern that became coarsening and thickening upward during the overlying highstand systems tract (HST). It consists of fine-grained turbidites (Facies V) and classical turbidites with wave reworked beds at the top (Facies VI) deposited in a shallow deltaic systems. Intervening postglacial brackish deposits contain an ichnofauna dominated by trackways of arthropods and minor grazing traces, preserved in bedding planes, that resemble nonmarine ichnocoenoses and differ from the archetypal brackish ichnofaunas, even when palynological data support the saline-depleted environment.

Registro:

Documento: Artículo
Título:The Late Carboniferous Glacial to Postglacial Transition: Facies and Sequence Stratigraphy, Western Paganzo Basin, Argentina
Autor:Pazos, P.J.
Filiación:Dpto. Ciencias Geológicas, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad de Buenos Aires 1428, Argentina
Palabras clave:Carboniferous; Glaciation; Gondwana; Ichnology; Sequence stratigraphy
Año:2002
Volumen:5
Número:2
Página de inicio:467
Página de fin:487
DOI: http://dx.doi.org/10.1016/S1342-937X(05)70736-X
Título revista:Gondwana Research
Título revista abreviado:Gondwana Res.
ISSN:1342937X
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1342937X_v5_n2_p467_Pazos

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Citas:

---------- APA ----------
(2002) . The Late Carboniferous Glacial to Postglacial Transition: Facies and Sequence Stratigraphy, Western Paganzo Basin, Argentina. Gondwana Research, 5(2), 467-487.
http://dx.doi.org/10.1016/S1342-937X(05)70736-X
---------- CHICAGO ----------
Pazos, P.J. "The Late Carboniferous Glacial to Postglacial Transition: Facies and Sequence Stratigraphy, Western Paganzo Basin, Argentina" . Gondwana Research 5, no. 2 (2002) : 467-487.
http://dx.doi.org/10.1016/S1342-937X(05)70736-X
---------- MLA ----------
Pazos, P.J. "The Late Carboniferous Glacial to Postglacial Transition: Facies and Sequence Stratigraphy, Western Paganzo Basin, Argentina" . Gondwana Research, vol. 5, no. 2, 2002, pp. 467-487.
http://dx.doi.org/10.1016/S1342-937X(05)70736-X
---------- VANCOUVER ----------
Pazos, P.J. The Late Carboniferous Glacial to Postglacial Transition: Facies and Sequence Stratigraphy, Western Paganzo Basin, Argentina. Gondwana Res. 2002;5(2):467-487.
http://dx.doi.org/10.1016/S1342-937X(05)70736-X