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    Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/33356


    Title: Formation of the Taiwan island as a solitary wave along the Eurasian continental plate margin: Magnetic and seismological evidence
    Authors: Wang,CS;Huang,CP;Ke,LY;Chien,WJ;Hsu,SK;Shyu,CT;Cheng,WB;Lee,CS;Teng,LS
    Contributors: 地球物理研究所
    Keywords: CHI-CHI EARTHQUAKE;ARC-CONTINENT;SUTURE ZONE;WESTERN END;EVOLUTION;COLLISION;AREA;REGION;MODEL;SOUTH
    Date: 2002
    Issue Date: 2010-07-07 10:58:41 (UTC+8)
    Publisher: 中央大學
    Abstract: The Philippine Sea plate moves northwestward, with respect to the Eurasian plate, and produces the Ryukyu subduction system (including the Ryukyu trench, the Ryukyu arc and the Okinawa trough) and the Manila subduction system (including the Manila trench
    Relation: TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
    Appears in Collections:[地球物理研究所] 期刊論文

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