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Capítulo de Libro

Tectonic Setting of the Tordillo Formation in the Aconcagua Fold-and-Thrust Belt

Título del libro: Opening and Closure of the Neuquén Basin in the Southern Andes

Acevedo, Eliana BelénIcon ; Rosselot, Eduardo Agustín; Martos, Federico ExequielIcon ; Fennell, Lucas MartínIcon ; Naipauer, MaximilianoIcon ; Folguera Telichevsky, AndresIcon
Otros responsables: Kietzmann, Diego AlejandroIcon ; Folguera Telichevsky, AndresIcon
Fecha de publicación: 2020
Editorial: Springer
ISBN: 978-3-030-29679-7
Idioma: Inglés
Clasificación temática:
Geología

Resumen

At the northwestern Mendoza province, the Mesozoic infill of the Neuquén Basin is tectonically repeated in the Aconcagua fold-and-thrust belt. Particularly, the Tordillo Formation (commonly associated with the Kimmeridgian) represents a local low stand period of sea level, with mainly alluvial and fluvial sediments. Toward the western sector of the belt, it interfingers with volcanic and volcaniclastic materials and presents a marked increase in the thickness. This unit was studied in two localities at the Blanco River valley, at the undeformed sector and over the second thrust that produces a second repetition of the Upper Jurassic and Lower Cretaceous sequences in the Aconcagua fold-and-thrust belt. This transect exposes facies variations and a significant increase in thickness to the west. Additionally, provenance analysis and paleocurrent directions indicate that the sediment supply was located to the E-SE, and that the underlying units were exhumed at the time of deposition of the Late Jurassic red beds. A consistent thickness increment of the Upper Jurassic deposits to the west through the Aconcagua fold-and-thrust belt suggests that sedimentation was controlled by NNW-directed structures. This is also supported by facies analyses that demonstrate high topographic breaks affecting a smooth westdipping fluvial ramp toward the volcanic arc. These features support an extensional setting for the deposition of the Tordillo Formation at the latitudes of the Aconcagua fold-and-thrust belt, as other authors have proposed for the Malargüe fold-and-thrust belt to the south. Plate tectonic reconstructions suggest trench rollback during this time previous to the westward migration of the South American plate, which is consistent with the back-arc extension proposed in the previous works.
Palabras clave: Tordillo Formation , Río Damas Formation , Back-arc extension , Aconcagua fold-and-thrust belt
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info:eu-repo/semantics/restrictedAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Unported (CC BY-NC-SA 2.5)
Identificadores
URI: http://hdl.handle.net/11336/111974
URL: https://link.springer.com/chapter/10.1007%2F978-3-030-29680-3_7
DOI: http://dx.doi.org/10.1007/978-3-030-29680-3_7
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Capítulos de libros(IDEAN)
Capítulos de libros de INSTITUTO DE ESTUDIOS ANDINOS "DON PABLO GROEBER"
Citación
Acevedo, Eliana Belén; Rosselot, Eduardo Agustín; Martos, Federico Exequiel; Fennell, Lucas Martín; Naipauer, Maximiliano; et al.; Tectonic Setting of the Tordillo Formation in the Aconcagua Fold-and-Thrust Belt; Springer; 2020; 159-174
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