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    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/103640


    Title: From submarine continental accretion to arc-continent orogenic evolution: The thermal record in southern Taiwan
    Authors: 林殿順;Mesalles, Lucas;Mouthereau, Frédéric;Bernet, Matthias;Chang, Chung-Pai;Lin, Andrew Tien-Shun;Fillon, Charlotte;Sengelen, Xavier
    Contributors: 地球科學學院地球科學學系
    Keywords: Acceleration;apatite;Asia;Cenozoic;cooling;Earth Sciences;Eurasian Plate;Evolution;exhumation;Far East;fission-track dating;Geochemistry;geochronology;Geophysics;metamorphic rocks;metasedimentary rocks;nesosilicates;Oceanography;orogenic belts;orthosilicates;Philippine Sea Plate;phosphates;plate collision;plate convergence;Plate tectonics;Pleistocene;Quaternary;Sciences of the Universe;Sedimentary geology;sedimentary rocks;silicates;solid Earth (tectonophysics);southern Taiwan;Taiwan;tectonics;Temperature effects;Tertiary;thermal history;zircon;zircon group
    Date: 2014-01-01
    Issue Date: 2026-04-23 11:34:25 (UTC+8)
    Publisher: Geological Society of America;Boulder: Geological Society of America (GSA)
    Abstract: 摘要: Constraining the timing of initial collision is critical for understanding how long-term plate convergence is accommodated at collisional plate boundaries. Reevaluation of the age of collision from orogenic thermal evolution requires distinguishing the onset of submarine continental accretion from earlier oceanic subduction and subsequent subaerial orogenic evolution. We present new thermochronological constraints from the first age-elevation relationship transect in Taiwan and zircon and apatite fission-track ages from sediments in the western foreland. Our data reveal the onset of cooling from at least 7.1 ± 1.3 Ma, at a minimum rate of 21 °C/m.y., in the submarine sedimentary wedge followed by a marked acceleration of subaerial exhumation after ca. 3.2 ± 0.6 Ma at an average rate of 1.7 km/m.y. Our data reflect the effect of margin architecture as Taiwan evolved from submarine accretion of the distal extremely thinned continental margin to crustal thickening of the proximal margin and orogenic development.
    出版者: Boulder: Geological Society of America (GSA)
    出版日期: 2014-10-01
    出處: Geology (Boulder), 2014-10, Vol.42 (10), p.907-910
    資源來源: GeoScienceWorld
    版權: GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from GeoScienceWorld Alexandria, VA USA United States. Reference includes data supplied by the Geological Society of America Boulder, CO USA United States
    版權: Copyright Geological Society of America Oct 2014
    版權: licence_http://creativecommons.org/publicdomain/zero
    識別號: ISSN: 0091-7613
    識別號: EISSN: 1943-2682
    識別號: DOI: 10.1130/G35854.1
    Appears in Collections:[Department of Earth Sciences ] journal & Dissertation

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