globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2020.116681
论文题名:
Deposition and erosion of a Light-Toned Yardang-forming unit of Mt Sharp, Gale crater, Mars
作者: Dromart G.; Le Deit L.; Rapin W.; Gasnault O.; Le Mouélic S.; Quantin-Nataf C.; Mangold N.; Rubin D.; Lasue J.; Maurice S.; Newsom H.E.; Pinet P.; Scuderi L.; Wiens R.C.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2021
卷: 554
语种: 英语
中文关键词: ChemCam ; Eolian ; Gale crater ; Mars climate ; stratigraphy ; yardang
英文关键词: Deposition ; Erosion ; Martian surface analysis ; Orbits ; Remote sensing ; Stratigraphy ; Structural geology ; Arid conditions ; Arid environments ; Climatic cycles ; Eolian deposition ; Geological units ; Mars science laboratory missions ; Remote sensing instruments ; Stratified rocks ; Climate change ; climate change ; crater ; deposition ; eolian deposit ; erosion ; Mars ; stratigraphy
英文摘要: Gale crater is a large impact crater with a ca 5 km thick sequence of stratified rocks in it, expressed today as a central eroded mound (i.e., Aeolis Mons informally named Mt. Sharp). A goal of the current Mars Science Laboratory mission in Gale crater is to investigate the processes that deposited, lithified, and eroded this fill. The Light-Toned Yardang Unit (LTYu) unit, the subject of the present research, is one of the geological units of Mt Sharp. Our specific purpose here is to refine and interpret the imaging documentation of the morphologic and stratal components of the LTYu, at large outcrop scale. In combination with established orbital images, we use the Remote Micro-Imager (RMI) of ChemCam, a remote sensing instrument currently operated onboard Curiosity rover, which provides several types of context imaging. RMI capabilities now include “Long Distance” acquisitions of targets several kilometers away. In these new acquisitions, substantial differences are visible in LTYu yardang attitudes from lowest to uppermost elevations allowing tentative subdivision of the LTYu into subunits. Bedding geometries in the lower LTYu are consistent with eolian dune foresets which collectively prograde towards an average N134° direction. Based on stratal architectures, the LTYu is viewed as an amalgamated stack of at least two, and possibly four, ancient erg systems bounded by large deflationary “supersurfaces”. Observations point to a multistory generation of yardangs interpreted to have been successively buried during the stratigraphic building of Mt Sharp. We conclude that the successive sequences of eolian deposition-erosion recorded by the LTYu have been generated by cyclic changes from semi-arid to arid conditions, coupled in climatic cycles, including wind regime change. The regional unconformity that tops the Lower mound formation of Mt Sharp, and the subsequent emplacement of the LTYu, collectively express a clear tendency toward sustained arid environments for this region of Mars around the Early – Late Hesperian transition. Given the large time scale involved (i.e., a few tens of million years as a minimum), we consider it likely that the local evidence for increased aridity in the Mt Sharp stratigraphy is a manifestation of climate change affecting the whole planet. © 2020 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165452
Appears in Collections:气候变化与战略

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作者单位: Univ Lyon, ENSL, Univ Lyon 1, CNRS, LGL-TPE, Lyon, 69364, France; Univ Nantes, CNRS, LPG, Nantes, 44322, France; California Institute of Technology, GPS, Pasadena, CA 91125, United States; Univ Toulouse, CNRS, CNES, IRAP, Toulouse, 31400, France; Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, Villeurbanne, 69622, France; University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, CA 95064, United States; University of New Mexico, Institute of Meteoritics, Albuquerque, NM 87131, United States; University of New Mexico, Department of Earth & Planetary Sciences, Albuquerque, NM 87131, United States; Los Alamos National Laboratory, Los Alamos, NM 87544, United States

Recommended Citation:
Dromart G.,Le Deit L.,Rapin W.,et al. Deposition and erosion of a Light-Toned Yardang-forming unit of Mt Sharp, Gale crater, Mars[J]. Earth and Planetary Science Letters,2021-01-01,554
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