博碩士論文 103690606 完整後設資料紀錄

DC 欄位 語言
DC.contributor國際研究生博士學位學程zh_TW
DC.creator庫馬zh_TW
DC.creatorUtpal Kumaren_US
dc.date.accessioned2020-11-24T07:39:07Z
dc.date.available2020-11-24T07:39:07Z
dc.date.issued2020
dc.identifier.urihttp://ir.lib.ncu.edu.tw:444/thesis/view_etd.asp?URN=103690606
dc.contributor.department國際研究生博士學位學程zh_TW
DC.description國立中央大學zh_TW
DC.descriptionNational Central Universityen_US
dc.description.abstract地球物理觀測涵蓋廣泛的時間尺度範圍,從地震所產生能量的瞬間變化到地質時間尺 度的板塊變形。本論文呈現探索不同時間尺度工具、複雜模型、資料迭代分析過程在 地震學與大地測量學的應用。 首先我們探索地震資料應用的過程,並使用三個研究結果來闡述與反演移動振源與地 球構造的特徵性質。在第一項研究中,透過地震波和聲下波陣列數據,我們分辨出 2013 年台灣北海岸淡水鎮的神秘爆炸聲源為流星衝擊波信號,並應用基因演算法反演 隕石軌跡的最佳解。在第二項研究中,針對印度最西部省份古吉拉特邦的雷利波相速 度在 20 到 90 秒的寬頻範圍內進行相速度異常圖的分析,我們使用計算所得測站間的 頻散曲線,將每個周期獨立地反演成高解析度均向性與隨著方位角變化的非均向性相 速度圖,結果與已知同區域的地質構造特徵相當吻合。在第三項研究中,我們開發了 一個全自動程式庫進行接收函數與剪力波分離的計算,唯一手動部分是使用者提供輸 入參數。此程式庫從全球可用的資料中心搜尋與下載資料並分別計算接收函數與剪力 波分離的結果,產生具出版品質的圖集。此程式庫已應用在 USArray 資料進行接收函 數分析與德國的測站網資料進行剪力波分離測量。 最後,我們對連續全球定位系統資料(CGPS)中的高振幅、長周期、空間相干共模誤差 (CME)的起源進行研究,分析台灣 47 個 GPS 測站所記錄到十年的日地殼變形資料來了 解 CME 的起源,其季節性證明了氣象起源。使用經驗正交函數(EOFs)分析提取 CME,發現 CME 與時域和譜域中的大氣質量負荷位移顯著相關。zh_TW
dc.description.abstractGeophysical observations, ranging from transient earthquake oscillations to tectonic deformations at geological scales, lie in a broad temporal spectrum. The work presented in this dissertation explores the asynchronous tools and models for the complex and iterative data analysis procedures applied in the seismology and geodesy. First, we explore the procedures applied to the seismic data and illustrate using three studies to characterize and invert for the moving source and the Earth structure. In the first study, the mysterious explosion sounds heard in the coastal town of Tamsui in Taiwan in 2013 was identified in the seismic and infrasound array data and characterized as a meteor shockwave signal and the trajectory of the meteor is inverted using Genetic Algorithm optimization scheme. In the second study, Rayleigh wave phase velocity anomaly maps of Gujarat, a westernmost province in India, is explored in a broad spectrum of 20-90s. The computed inter-station dispersion curves are inverted for high-resolution isotropic and azimuthally anisotropic phase velocity maps at each period independently, coinciding well with the known geological features in the region. In the third study, a fully automated package is developed (in Python) to conduct the Receiver Functions (RF) and Shear-wave Splitting (SWS) computation for the user-provided input parameters (the only manual part). The dataset is automatically searched and downloaded from all the available data centers around the world and is processed, and computed for RF and SWS results independently along with high-resolution figures. The package is applied to the USArray data for the RF analysis and the networks around Germany for SWS measurements. Finally, a study is conducted to understand the origin of the high amplitude, long period, and spatially coherent common-mode error (CME) in continuous GPS (CGPS) data. Ten years of daily crustal deformations recorded at 47 CGPS stations in Taiwan are analyzed to understand the origin of CME whose seasonality evidences meteorological origin. CME is extracted using the Empirical Orthogonal Functions (EOFs) analysis and found to be significantly correlated with the atmospheric mass loading displacements in both temporal and spectral domains.en_US
DC.subject地震学zh_TW
DC.subject大地测量学zh_TW
DC.subject流星冲击波zh_TW
DC.subject表面波层析成像zh_TW
DC.subject共模误差zh_TW
DC.subjectSTADIUMpyzh_TW
DC.subjectSeismologyen_US
DC.subjectGeodesyen_US
DC.subjectMeteor Shockwaveen_US
DC.subjectSurface wave Tomographyen_US
DC.subjectCommon-mode Erroren_US
DC.subjectSTADIUMpyen_US
DC.title地球物理資料分析在地震學與測地學的應用zh_TW
dc.language.isozh-TWzh-TW
DC.titleSeismological and Geodetic Applications of Geophysical Data Analysisen_US
DC.type博碩士論文zh_TW
DC.typethesisen_US
DC.publisherNational Central Universityen_US

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