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Abstract:

Detrital modes of sandstones and conglomerates of the Toro Negro Formation (Late Miocene-early Pliocene) were used to analyze the evolution of the broken-foreland stage of the Vinchina Basin (28°30'-29°00' S and 68°30'-68°20' W) of NW Argentina. This basin located in the Western Sierras Pampeanas is bounded to the west by the Precordillera and to the east by the Famatina System. Three sandstone petrofacies: plutonic-metamorphic, volcanic and mixed petrofacies and three conglomerate lithic associations: basement, sedimentary and volcanic lithic associations were recognized, allowing to establish three source areas: Western Sierras Pampeanas (Toro Negro and Umango Ranges), Cordillera Frontal and Precordillera.During the Late Miocene, the Toro Negro Range (to the north) together with the Cordillera Frontal and Precordillera (to the west) were the main sources for depositional sequences I and II (lower member of the Toro Negro Formation). On the contrary, during the latest Miocene-early Pliocene, Depositional Sequence III (upper member) exhibited a progressive increase in the supply from the eastern Precordillera (to the west) with additional material from the Umango Range to the south. Besides, evidence of synchronic volcanism is recorded in the upper part of Depositional Sequence II and the lower part of Depositional Sequence III.The coexistence of the three source areas and the changing distribution patterns due to re-accommodation of sediment dispersal routes demonstrate that the evolution of this type of basin is much more complex than previously envisaged. Therefore, an integrated analysis using different tools (sedimentary facies, paleocurrent measurements, sandstone petrography and conglomerate composition) is needed for a clearer understanding of broken-foreland basins. © 2013 Elsevier Ltd.

Registro:

Documento: Artículo
Título:Petrology and provenance of the Toro Negro Formation (Neogene) of the Vinchina broken-foreland basin (Central Andes of Argentina)
Autor:Ciccioli, P.L.; Marenssi, S.A.; Limarino, C.O.
Filiación:Departamento de Ciencias Geológicas, IGeBA, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, CONICET, Ciudad Universitaria, Pabellón 2, 1 piso, C1428EHA Buenos Aires, Argentina
Idioma: Inglés
Palabras clave:Andes; Broken-foreland; Neogene; Petrofacies; Sedimentary petrology; basin evolution; conglomerate; depositional sequence; detrital deposit; foreland basin; lithostratigraphy; Neogene; provenance; sandstone; sedimentary petrology; Andes; Argentina; Cordillera Frontal; Precordillera; Sierras Pampeanas
Año:2014
Volumen:49
Página de inicio:15
Página de fin:38
DOI: http://dx.doi.org/10.1016/j.jsames.2013.10.003
Título revista:Journal of South American Earth Sciences
Título revista abreviado:J. South Am. Earth Sci.
ISSN:08959811
Registro:http://digital.bl.fcen.uba.ar/collection/paper/document/paper_08959811_v49_n_p15_Ciccioli

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Citas:

---------- APA ----------
Ciccioli, P.L., Marenssi, S.A. & Limarino, C.O. (2014) . Petrology and provenance of the Toro Negro Formation (Neogene) of the Vinchina broken-foreland basin (Central Andes of Argentina). Journal of South American Earth Sciences, 49, 15-38.
http://dx.doi.org/10.1016/j.jsames.2013.10.003
---------- CHICAGO ----------
Ciccioli, P.L., Marenssi, S.A., Limarino, C.O. "Petrology and provenance of the Toro Negro Formation (Neogene) of the Vinchina broken-foreland basin (Central Andes of Argentina)" . Journal of South American Earth Sciences 49 (2014) : 15-38.
http://dx.doi.org/10.1016/j.jsames.2013.10.003
---------- MLA ----------
Ciccioli, P.L., Marenssi, S.A., Limarino, C.O. "Petrology and provenance of the Toro Negro Formation (Neogene) of the Vinchina broken-foreland basin (Central Andes of Argentina)" . Journal of South American Earth Sciences, vol. 49, 2014, pp. 15-38.
http://dx.doi.org/10.1016/j.jsames.2013.10.003
---------- VANCOUVER ----------
Ciccioli, P.L., Marenssi, S.A., Limarino, C.O. Petrology and provenance of the Toro Negro Formation (Neogene) of the Vinchina broken-foreland basin (Central Andes of Argentina). J. South Am. Earth Sci. 2014;49:15-38.
http://dx.doi.org/10.1016/j.jsames.2013.10.003