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• W2089690388 abstract "Abstract The study of the Las Tunas River incisions, located in the eastern Andean foreland front (33 20’ S in Argentina), provides new clues for the interpretation of deep piedmont entrenchments. Both the Las Tunas mountain catchment and its piedmont are strongly entrenched with maximal incision of over 100 m at the mountain front. Three main terrace levels are well exposed and are labelled T1, T2 and T3 from the youngest to the oldest. We combined geological and geomorphological field observations, kinematic GPS data, satellite data and aerial photos with geochronological and analysis to provide a detailed description of terrace organization and a discussion of the evolution of the Las Tunas landscape. The surprisingly constant concentrations in surface layers as deep as 1.5 m show that gently dipping alluvial surfaces can be continuously and deeply mixed. Our data show a first period of deposition (Mesones Fm) before 0.85 Myr (minimum T3 age), followed by deep erosion and a second sedimentation period (Las Tunas Fm) that includes a ca. 0.6 Myr ash deposit. T2 and T1 are inset in the Las Tunas Fm and were abandoned ca. 15–20 kyr ago. The similar ages for T2 and T1 show that post‐20 kyr entrenchment occurred very rapidly. Despite Quaternary deformation in the Las Tunas piedmont, terrace entrenchment is best explained by paleo‐climatic changes. The terrace organization reveals that the erosion‐sedimentation phases affected the entire system from the piedmont toe to 10 km upstream of the mountain front. Finally, contrary to the neighbouring more deeply incised Diamante River system, where late Quaternary piedmont uplift is more likely to have been a factor causing incision, the more stable Las Tunas system provides an incomplete geomorphological record of Pleistocene and Holocene climate variations. We suggest that climate variations are better recorded in uplifting piedmonts than in stable ones, where the magnitude of incision and sedimentation and the fact that they occur repeatedly at the same elevation can erase a large part of the record." @default.
• W2089690388 created "2016-06-24" @default.
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• W2089690388 date "2013-05-25" @default.
• W2089690388 modified "2023-10-16" @default.
• W2089690388 title "Pleistocene landscape entrenchment: a geomorphological mountain to foreland field case, the Las Tunas system, Argentina" @default.
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• W2089690388 cites W1534673777 @default.
• W2089690388 cites W1558473326 @default.
• W2089690388 cites W1587525523 @default.
• W2089690388 cites W1638691163 @default.
• W2089690388 cites W1894241181 @default.
• W2089690388 cites W1965832912 @default.
• W2089690388 cites W1969252712 @default.
• W2089690388 cites W1970983096 @default.
• W2089690388 cites W1972230154 @default.
• W2089690388 cites W1972341769 @default.
• W2089690388 cites W1976259033 @default.
• W2089690388 cites W1978299336 @default.
• W2089690388 cites W1987844701 @default.
• W2089690388 cites W1989875050 @default.
• W2089690388 cites W1994091335 @default.
• W2089690388 cites W1995040253 @default.
• W2089690388 cites W1998090707 @default.
• W2089690388 cites W2001664107 @default.
• W2089690388 cites W2005035365 @default.
• W2089690388 cites W2007147137 @default.
• W2089690388 cites W2007324355 @default.
• W2089690388 cites W2007609987 @default.
• W2089690388 cites W2008067782 @default.
• W2089690388 cites W2009425598 @default.
• W2089690388 cites W2015136608 @default.
• W2089690388 cites W2016029130 @default.
• W2089690388 cites W2016055802 @default.
• W2089690388 cites W2016138287 @default.
• W2089690388 cites W2020255158 @default.
• W2089690388 cites W2020316882 @default.
• W2089690388 cites W2022796365 @default.
• W2089690388 cites W2025997795 @default.
• W2089690388 cites W2026049456 @default.
• W2089690388 cites W2026999407 @default.
• W2089690388 cites W2027336503 @default.
• W2089690388 cites W2027424149 @default.
• W2089690388 cites W2027913477 @default.
• W2089690388 cites W2031178854 @default.
• W2089690388 cites W2035932728 @default.
• W2089690388 cites W2036024673 @default.
• W2089690388 cites W2037553700 @default.
• W2089690388 cites W2045172449 @default.
• W2089690388 cites W2060207812 @default.
• W2089690388 cites W2061623896 @default.
• W2089690388 cites W2063155650 @default.
• W2089690388 cites W2069193736 @default.
• W2089690388 cites W2070984609 @default.
• W2089690388 cites W2074297072 @default.
• W2089690388 cites W2074819215 @default.
• W2089690388 cites W2074925658 @default.
• W2089690388 cites W2080171944 @default.
• W2089690388 cites W2084744129 @default.
• W2089690388 cites W2090791965 @default.
• W2089690388 cites W2093570562 @default.
• W2089690388 cites W2095194310 @default.
• W2089690388 cites W2095358378 @default.
• W2089690388 cites W2107213367 @default.
• W2089690388 cites W2115063257 @default.
• W2089690388 cites W2122814825 @default.
• W2089690388 cites W2127335932 @default.
• W2089690388 cites W2130049326 @default.
• W2089690388 cites W2134111740 @default.
• W2089690388 cites W2134873983 @default.
• W2089690388 cites W2143020040 @default.
• W2089690388 cites W2145216970 @default.
• W2089690388 cites W2148162674 @default.
• W2089690388 cites W2149128668 @default.
• W2089690388 cites W2150821916 @default.
• W2089690388 cites W2615915854 @default.
• W2089690388 cites W4245230373 @default.
• W2089690388 doi "https://doi.org/10.1111/bre.12019" @default.
• W2089690388 hasPublicationYear "2013" @default.
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