Title page for 956204004


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Student Number 956204004
Author Shih-wai Shen(沈士崴)
Author's Email Address No Public.
Statistics This thesis had been viewed 1855 times. Download 336 times.
Department Graduate Institute of Applied Geology
Year 2007
Semester 2
Degree Master
Type of Document Master's Thesis
Language zh-TW.Big5 Chinese
Title 3D Shear-wave Velocity Structure of Songshan Formation, Taipei Basin.
Date of Defense 2008-07-09
Page Count 81
Keyword
  • cokriging
  • shear-wave velocity
  • Songshan Formation
  • Taipei basin
  • Abstract This study estimates shear-wave velocity structure of Songshan Formation in Taipei basin using shear-wave velocity data and standard penetration test data (SPT-N) from boring and testing data at free-field strong-motion station sites and Geo2005 database, and other sources. Geostatistical analysis of semivariograms and cross-semivariograms in 3D and cokriging method was used for the estimation.
     Structural analyses of shear-wave velocity data and SPT-Ns show good spatial relations in each semivariogram and cross-semivariogram. Therefore, shear-wave velocity was used as a primary variable and SPT-N as a secondary variable in the cokriging method. The result is a 3D regular grid digital model, and is shown by a set of contour maps and profile maps.
     Shear-wave velocity value in the Songshan Formation increases with depth; it is about 100~200m/s within 10m depth and increases to 400~500m/s at about 45m depth. Horizontal variation of Shear-wave velocities may be shown by the variation of average shear-wave velocity within 30m depth (Vs30). The Vs30 map shows low value (160~180m/s) at Zhongshan District, and shows moderately low value (180~200m/s) at Beitou, Shilin, Datong, Zhongshan, Zhongzheng, Daan, Xinyi, Songshan District and Sanchong City. Shear-wave velocities increase from the above-mentioned low and moderately-low zones to the southwest, and reach a moderate value (220~240m/s) at Sinjhuang, Banciao, Junghe and Yunghe. It reaches 260m/s at Shulin and Tucheng. Result of this study is similar with previous researches in general, but it shows more details and lower estimation error in the variation of shear-wave velocities.
    Table of Content 目 錄........................................................................................V
    圖 目......................................................................................VII
    表 目........................................................................................X
    第1章 緒論.............................................................................1
    1.1 研究動機與目的.....................................................................1
    1.2 文獻回顧.................................................................................1
    1.3 研究區域簡介.........................................................................2
    1.4 研究架構與流程.....................................................................7
    第2章 研究方法......................................................................7
    2.1 地質統計學原理.......................................................................7
    2.2 地質統計學內插方法...............................................................7
    2.2.1 聯合克力金法................................................................7
    第3章 資料蒐集與處理........................................................10
    3.1 研究資料蒐集與處理.............................................................10
    3.1.1 強震測站場址工程地質鑽探資料..............................10
    3.1.2 國土資訊系統工程地質鑽探資料..............................10
    3.1.3 中央大學應用地質所工程地質研究室台北盆地鑽探資料庫..........................................................................10
    3.2 資料篩選檢核.........................................................................12
    第4章 剪力波速度三維空間推估........................................14
    4.1 基本資料統計.........................................................................14
    4.1.1 剪力波速度資料基本統計..........................................14
    4.1.2 標準貫入試驗資料基本統計......................................15
    4.2 剪力波速度資料與標準貫入試驗值資料空間分析.............15
    4.2.1 剪力波速度資料半變異圖分析..................................15
    4.2.2 標準貫入試驗資料半變異圖分析..............................17
    4.3 台北盆地剪力波速度與標準貫入試驗資料相關性分析.....18
    4.3.1 迴歸分析......................................................................18
    4.3.2 交叉半變異圖分析......................................................19
    4.4 鑽井孔口高程趨勢面.............................................................21
    4.4.1 趨勢面分析..................................................................22
    4.4.2 趨勢面使用..................................................................22
    4.5 搜尋半徑.................................................................................23
    4.6 研究結果.................................................................................24
    第5章 討論............................................................................51
    5.1 與「台北盆地松山層土壤性質之空間分析」比較.................51
    5.1.1 內插方法比較..............................................................51
    5.1.2 內插結果比較..............................................................52
    5.2 與「臺灣自由場強震站場址分類之進一步研究」比較.........66
    5.2.1 內插方法比較..............................................................66
    5.2.2 內插結果比較..............................................................66
    5.3 交叉驗證.................................................................................68
    第6章 結論與建議................................................................72
    6.1 結論.........................................................................................72
    6.2 建議.........................................................................................72
    參考文獻...................................................................................74
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  • Chyi-Tyi Lee(李錫堤)
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    Date of Submission 2008-07-22

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