Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains

碩士 === 國立中央大學 === 地球物理研究所 === 100 === I used the PSInSAR and Small baseline techniques to investigate the surface deformation of the northern Taiwan area, including the Taipei basin and its surrounding mountain areas. Integrating the Persistent Scatterer Interferometry (PSInSAR) and Small baseline s...

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Main Authors: Kai-Ting Fan, 范凱婷
Other Authors: Horng-Yuan Yen
Format: Others
Language:zh-TW
Published: 2012
Online Access:http://ndltd.ncl.edu.tw/handle/06048174448919773064
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spelling ndltd-TW-100NCU051340102015-10-13T21:22:38Z http://ndltd.ncl.edu.tw/handle/06048174448919773064 Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains 台北盆地及周圍山區之現今地表變形研究 Kai-Ting Fan 范凱婷 碩士 國立中央大學 地球物理研究所 100 I used the PSInSAR and Small baseline techniques to investigate the surface deformation of the northern Taiwan area, including the Taipei basin and its surrounding mountain areas. Integrating the Persistent Scatterer Interferometry (PSInSAR) and Small baseline subset InSAR (SBAS) results, I observed some deformation events in northern Taiwan including: 1) The Taipei basin had experienced uplift from 1993 to 2001, which may relate to aquifer rebound. 2) In contrast the Taipei basin had subsided from 2003 to 2008 possibly due to massive pumping of groundwater. 3) In the western of Taipei basin, the ground subsidence from 1993 to 2008 may be caused by the compaction of shallow sediments and interseismic deformation of the Sanchiao fault. 4) The Da-You-Kan area had been uplifted from 2003 to 2008 that may be caused by magmatic or geothermal activities. Further comparisons between the PSInSAR, Small baseline, and the corresponding leveling data show a coincident pattern, and therefore largely improve the authenticity of radar interferometry. Horng-Yuan Yen Chung-Pai Chang 顏宏元 張中白 2012 學位論文 ; thesis 102 zh-TW
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language zh-TW
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description 碩士 === 國立中央大學 === 地球物理研究所 === 100 === I used the PSInSAR and Small baseline techniques to investigate the surface deformation of the northern Taiwan area, including the Taipei basin and its surrounding mountain areas. Integrating the Persistent Scatterer Interferometry (PSInSAR) and Small baseline subset InSAR (SBAS) results, I observed some deformation events in northern Taiwan including: 1) The Taipei basin had experienced uplift from 1993 to 2001, which may relate to aquifer rebound. 2) In contrast the Taipei basin had subsided from 2003 to 2008 possibly due to massive pumping of groundwater. 3) In the western of Taipei basin, the ground subsidence from 1993 to 2008 may be caused by the compaction of shallow sediments and interseismic deformation of the Sanchiao fault. 4) The Da-You-Kan area had been uplifted from 2003 to 2008 that may be caused by magmatic or geothermal activities. Further comparisons between the PSInSAR, Small baseline, and the corresponding leveling data show a coincident pattern, and therefore largely improve the authenticity of radar interferometry.
author2 Horng-Yuan Yen
author_facet Horng-Yuan Yen
Kai-Ting Fan
范凱婷
author Kai-Ting Fan
范凱婷
spellingShingle Kai-Ting Fan
范凱婷
Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
author_sort Kai-Ting Fan
title Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
title_short Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
title_full Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
title_fullStr Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
title_full_unstemmed Study of Recent Surface Deformation in Taipei basin and Its Surrounding Mountains
title_sort study of recent surface deformation in taipei basin and its surrounding mountains
publishDate 2012
url http://ndltd.ncl.edu.tw/handle/06048174448919773064
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