Arid
DOI10.1016/j.geomorph.2021.107747
Erosion around a large-scale topographic high in a semi-arid sedimentary basin: Interactions between fluvial erosion, aeolian erosion and aeolian transport
Jolivet, M.; Braucher, R.; Dovchintseren, D.; Hocquet, S.; Schmitt, J. -M.
通讯作者Jolivet, M (corresponding author), Univ Rennes, CNRS, UMR6118, Geosci Rennes, F-35000 Rennes, France.
来源期刊GEOMORPHOLOGY
ISSN0169-555X
EISSN1872-695X
出版年2021
卷号386
英文摘要Large-scale aeolian erosion features such as pans usually develop upon a relatively homogeneous erodible sedimentary rock substratum and show simple concave morphologies. However, some erosional depressions in semi-arid to arid settings develop in more complex geological contexts, associating sedimentary basins and outcrops of non-erodible basement. In semi-arid basins, the geomorphic evolution is controlled by interplay between the processes of fluvial erosion and deposition (especially of the finer sediment fraction in ephemeral lakes) and the processes of aeolian erosion and deflation. The occurrence of non-erodible basement outcrops within a region of overall deflation complicates drainage systems and wind-flow patterns. Both are liable to evolve rapidly through time and their interactions remain poorly understood. In this study, we use a detailed geomorphological analysis, including mapping of the aeolian sand-motion direction within the 16,300 km(2) Tsagaan Els depression (Gobi Desert, Mongolia) as well as in situ-produced cosmogenic Be-10 and Al-26 based quantitative constraints, to propose a conceptual model for the morphologic evolution of geologically complex semi-arid basins. Based on theoretical studies of wind-flow patterns around obstacles, we demonstrate that the occurrence of erosion-resistant basement highs inside the basin induces the localization of preferential deflation zones and aeolian and fluvial carving of large-scale relief. The enhanced deflation zones form sub-depocenters controlling local drainage systems that mobilize clastic material and transport it to the deflation zone. These river systems are frequently captured by neighboring streams, which creates unstable conditions of erosion and deposition. Such rapid modifications of the topography through time affect the hydrogeologic structure of the basin and may impact potential sediment-hosted mineral deposits. (C) 2021 Elsevier B.V. All rights reserved.
英文关键词Aeolian erosion Fluvial-aeolian interaction Aeolian geomorphology Cosmogenic radionuclides Gobi desert
类型Article
语种英语
开放获取类型Green Published
收录类别SCI-E
WOS记录号WOS:000655695000002
WOS关键词CENTRAL PANNONIAN BASIN ; EAST GOBI BASIN ; QATTARA DEPRESSION ; STRUCTURAL RECORDS ; DUST DEPOSITION ; INNER-MONGOLIA ; COLORADO RIVER ; MOJAVE DESERT ; SAND DUNES ; HALF-LIFE
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
来源机构French National Research Institute for Sustainable Development ; E17
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350416
作者单位[Jolivet, M.; Dovchintseren, D.] Univ Rennes, CNRS, UMR6118, Geosci Rennes, F-35000 Rennes, France; [Braucher, R.; Hocquet, S.; Schmitt, J. -M.; ASTER Team] Aix Marseille Univ, CNRS, UMR34 CEREGE, IRD,Coll France,INRAE, Technopole Environm Arbois & Mediterranee,BP80, F-13545 Aix En Provence, France; [Dovchintseren, D.] Orano Min, 1 Pl J Millier, F-92400 Courbevois, France
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GB/T 7714
Jolivet, M.,Braucher, R.,Dovchintseren, D.,et al. Erosion around a large-scale topographic high in a semi-arid sedimentary basin: Interactions between fluvial erosion, aeolian erosion and aeolian transport[J]. French National Research Institute for Sustainable Development, E17,2021,386.
APA Jolivet, M.,Braucher, R.,Dovchintseren, D.,Hocquet, S.,&Schmitt, J. -M..(2021).Erosion around a large-scale topographic high in a semi-arid sedimentary basin: Interactions between fluvial erosion, aeolian erosion and aeolian transport.GEOMORPHOLOGY,386.
MLA Jolivet, M.,et al."Erosion around a large-scale topographic high in a semi-arid sedimentary basin: Interactions between fluvial erosion, aeolian erosion and aeolian transport".GEOMORPHOLOGY 386(2021).
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