Formation of the Taiwan island as a solitary wave along the Eurasian continental plate margin: Magnetic and seismological evidence

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題名:	Formation of the Taiwan island as a solitary wave along the Eurasian continental plate margin: Magnetic and seismological evidence
作者:	Wang,CS;Huang,CP;Ke,LY;Chien,WJ;Hsu,SK;Shyu,CT;Cheng,WB;Lee,CS;Teng,LS
貢獻者:	地球物理研究所
關鍵詞:	CHI-CHI EARTHQUAKE;ARC-CONTINENT;SUTURE ZONE;WESTERN END;EVOLUTION;COLLISION;AREA;REGION;MODEL;SOUTH
日期:	2002
上傳時間:	2010-07-07 10:58:41 (UTC+8)
出版者:	中央大學
摘要:	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
關聯:	TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
顯示於類別:	[地球物理研究所] 期刊論文

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