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

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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:	[Graduate Institute of Geophysics] journal & Dissertation

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