Melting features along the western Ryukyu slab edge (northeast Taiwan): Tomographic evidence

NCUIR > College of Earth Sciences > Graduate Institute of Geophysics > journal & Dissertation > Item 987654321/33330

Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/33330

Title:	Melting features along the western Ryukyu slab edge (northeast Taiwan): Tomographic evidence
Authors:	Lin,JY;Hsu,SK;Sibuet,JC
Contributors:	地球物理研究所
Keywords:	BACK-ARC BASIN;V-P/V-S;OKINAWA TROUGH;TECTONIC IMPLICATIONS;SUBDUCTION ZONE;OBLIQUE SUBDUCTION;VELOCITY STRUCTURE;3-DIMENSIONAL P;MAGMA GENESIS;REGION
Date:	2004
Issue Date:	2010-07-07 10:57:49 (UTC+8)
Publisher:	中央大學
Abstract:	[1] Behind the sedimentary Ryukyu arc lies the Okinawa Trough, whose termination is located at the tip of the Ilan plain ( northern Taiwan), just above the Ryukyu slab edge. The present-day active volcanic front is located 80 - 100 km above the Ryukyu sla
Relation:	JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
Appears in Collections:	[Graduate Institute of Geophysics] journal & Dissertation

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