利用強地動資料層析花東縱谷速度構造;Using strong motion data to invert velocity structure in Longitudal Valley

NCUIR > College of Earth Sciences > Department of Earth Sciences > Research Project > Item 987654321/61960

Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/61960

Title:	利用強地動資料層析花東縱谷速度構造;Using strong motion data to invert velocity structure in Longitudal Valley
Authors:	陳伯飛
Contributors:	國立中央大學地球科學學系
Keywords:	地球科學
Date:	2014-03-11
Issue Date:	2014-03-11 13:07:50 (UTC+8)
Publisher:	交通部中央氣象局
Abstract:	研究期間：10302~10312;The Longitudal Valley in East Taiwan is the collision suture zone between the Philippine Sea Plat and the Eurasia Plate. The abundant seismic activity in the valley demonstrates different behaviors between the North and South segments. Furthermore, whether there is a west-dipping Central Range Fault in the valley remains an open question. Some areas in the longitudal valley possess potentials for geothermal explorations. In this proposal, we plan to conduct a tomographic study to invert high resolution crustal velocity structures in the Longitudal Valley using P and S arrival times as recorded by strong motion stations in the area deployed by Central Weather Bureau over the past decade or so. The resulting velocity structures can be used to correlate with the N-S different seismic behaviors, to detect the potential existence of the Central Range Fault, and to determine the suitable sites for geothermal explorations. We expect that fulfillment of the project will significantly help understand the seismotectonics of the Longitudal Valley for a better prediction on potential zones of future earthquakes for hazard mitigation.
Relation:	財團法人國家實驗研究院科技政策研究與資訊中心
Appears in Collections:	[Department of Earth Sciences ] Research Project

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