How was Taiwan created?

NCUIR > College of Earth Sciences > Graduate Institute of Geophysics > journal & Dissertation > Item 987654321/33325

Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/33325

Title:	How was Taiwan created?
Authors:	Sibuet,JC;Hsu,SK
Contributors:	地球物理研究所
Keywords:	ARC-CONTINENT COLLISION;PHILIPPINE SEA PLATE;1999 CHI-CHI;TECTONIC EVOLUTION;OBLIQUE SUBDUCTION;MAGNETIC-ANOMALIES;RYUKYU SUBDUCTION;OKINAWA TROUGH;MOUNTAIN BELT;SHIKOKU BASIN
Date:	2004
Issue Date:	2010-07-07 10:57:35 (UTC+8)
Publisher:	中央大學
Abstract:	Since the beginning of formation of proto-Taiwan during late Miocene (9 Ma), the subducting Philippine (PH) Sea plate moved continuously through time in the N307degrees direction at a 5.6 cm/year velocity with respect to Eurasia (EU), tearing the Eurasian
Relation:	TECTONOPHYSICS
Appears in Collections:	[Graduate Institute of Geophysics] journal & Dissertation

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