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- W2117546572 abstract "The Rio del Penon Formation (Borrello, 1955 nom. subst. Gonzalez y Bossi, 1986) forms the upper part of the late Paleozoic outcropping in the Rio Blanco anticline (northwest Precordillera, La Rioja Province). This unit is predominantly composed of a thick (1270 m.) sandstone and mudstone sequence including thin levels of coal and scarce conglomerates (Scalabrini Ortiz, 1972; Scalabrini Ortiz and Arrondo, 1973; Gonzalez and Bossi, 1986). These deposits represent a complex interfingering of shallow marine and fluvial deposits recording relative sea-level fluctuations during the Late Carboniferous-Early Permian. The Rio del Penon Formation overlies andesites and volcanic breccias of the Punta del Agua Formation (Fig. 1 and 2a).Despite well known Late Carboniferous glacigenic deposits from different localities within the Precordillera (Lopez Gamundi, 1987, 1997; Lopez Gamundi and Martinez, 2000; Marenssi et al., 2004; Limarino and Spalletti, 2006; Henry et al., in press), glaciogenic deposits have not been reported from the Rio del Penon Formation. This documentation of glacial-related sediments in this succession serves to further constrain our knowledge of the temporal and paleogeographic distribution of Gondwanan glacial deposits." @default.
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- W2117546572 date "2008-07-01" @default.
- W2117546572 modified "2023-09-23" @default.
- W2117546572 title "Glacial Deposits in the Río del Peñón Formation (Late Carboniferous), Río Blanco Basin, Northwestern Argentina" @default.
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