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    請使用永久網址來引用或連結此文件: https://irlib.pccu.edu.tw/handle/987654321/29185


    題名: How fast is the denudation of the Taiwan mountain belt? Perspectives from in situ cosmogenic Be-10
    作者: Derrieux, Florence
    Siame, Lionel L.
    Bourles, Didier L.
    Chen, Rou-Fei
    Braucher, Regis
    Leanni, Laetitia
    Lee, Jian-Cheng
    Chu, Hao-Tsu
    Byrne, Timothy B.
    貢獻者: 地質系
    關鍵詞: Denudation
    Cosmogenic nuclides [Be-10]
    Mountain building
    Taiwan
    日期: 2014-07
    上傳時間: 2015-01-26 09:20:15 (UTC+8)
    摘要: Quantifying denudation rates in a wide range of climatic and tectonic settings at various time and space scales is a critical step in calibrating and validating landscape evolution models. Focusing on Taiwan, we quantified centennial rates of denudation at the scale of the whole orogen, using in situ Be-10 concentrations measured in stream sediments collected at the outlets of major rivers. To assess denudation rates that are statistically significant, we applied both the mean square weighted deviation approach and the bootstrap technique. For the central segment of the belt, where the collision is considered to be near mature, the orogen-scale pattern of denudation shows a two-fold pattern: (1) higher denudation values on the order of 4-5 mm/yr characterize the eastern side of the belt (i.e., retro-wedge), with a slight increase towards the south and (2) lower denudation values on the order of,1-3 mm/yr on the western side of the belt (pro-wedge) with a minimum value centered on the main recess of the deformation front. To the north and to the south of the central segment, the denudation rates converge towards lower values on the order of 2-3 mm/yr. At the scale of the mountain belt, drainage basin metrics such as relief, hypsometric index and slope values seem to explain the observed variance in the data population, conversely to the first-order average precipitation pattern, suggesting a strong tectonic control on the regional pattern of denudation rates. Applied to the whole orogen, such field-based approach thus provides important input data to validate and calibrate the parameters to be supplied to landscape evolution models. (c) 2014 Elsevier Ltd. All rights reserved.
    關聯: JOURNAL OF ASIAN EARTH SCIENCES 卷: 88 頁碼: 230-245
    顯示於類別:[地質系] 期刊論文

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