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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 吳逸民(Yih-Min Wu) | |
dc.contributor.author | Han-Yu Huang | en |
dc.contributor.author | 黃翰榆 | zh_TW |
dc.date.accessioned | 2021-06-16T06:41:17Z | - |
dc.date.available | 2015-08-08 | |
dc.date.copyright | 2014-08-08 | |
dc.date.issued | 2014 | |
dc.date.submitted | 2014-07-29 | |
dc.identifier.citation | Akuhara, T., Mochizuki, K., Nakahigashi, K., Yamada, T., Shinohara, M., Sakai, S.i., . . . Shimizu, H. (2013). Segmentation of the Vp/Vs ratio and low-frequency earthquake distribution around the fault boundary of the Tonankai and Nankai earthquakes. Geophysical Research Letters,40, 1306-1310.
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H., Chen, Y.-G., Sieh, K., & Avouac, J.-P. (2007). Seismic tomography of Taiwan: Improved constraints from a dense network of strong motion stations. Journal of Geophysical Research, 112, B08312 Wu, Y.-M., Shyu, J. B. H., Chang, C.-H., Zhao, L., Nakamura, M., & Hsu, S.-K. (2009). Improved seismic tomography offshore northeastern Taiwan: implications for subduction and collision processes between Taiwan and the southernmost Ryukyu. Geophysical Journal International, 178, 1042-1054. 中文部分 周心怡,2004,拔靴法之探討及其應用,國立中央大學統計研究所,碩士論文。 干裕成,2004,劣化混凝土材料應力波傳速度與E 值、老化時程及抗壓強度之 關係,行政院原子能委員會委託研究計畫研究報告。 張育群,2013,建置台灣重複地震自動化偵測系統,國立台灣師範大學地球科學 系,碩士論文。 劉瀚方,2013,清水地熱地區之微震與震波走時層析成像,國立台灣大學地質科學所,碩士論文。 線上資源 https://pangea.stanford.edu/~jack/JD_Course_2008b.pdf(史丹佛大學課程教學網) | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/57312 | - |
dc.description.abstract | 現今,大家普遍使用地震的走時資料來逆推出震波層析成像 ( Seismic Tomography) 並得出Vp/Vs值。但是,因為網格化與逆推方法的使用,讓層析成像大多使用於大構造上的解析。有鑑於此,Lin and Shearer (2007)提出了套新的方法,透過利用相似地震群內的波形資料,藉由波形的交叉相關法可以量測到P波與S波的到時差異來計算出Vp/Vs值。這個新的技術,也被前人證明具有計算出高解析度Vp/Vs值的能力。台灣地區位在地震密集的板塊交界帶上,而有豐富的地震資料。加上,近年來不同觀測網的建立,讓台灣能夠擁有包覆度很高的地震監測網。在具備了上述條件之下,這個新的Vp/Vs值計算方法是非常適合在台灣地區進行測試的。但是,考量到台灣地下構造的複雜程度與前人所研究的美國南加州區域有明顯差異,必須先對這個新的方法針對不同的因素、參數與區域進行測試。之後,才能將測試結果應用在台灣的相似地震序列的波形資料上。因此,本研究對不同的因素與參數進行測試,加上修改前人所發展的回歸方法,成功地將迴歸流程使用在真實的相似地震資料上,並計算出了高精準度的Vp/Vs值。與震波層析成像的結果一起分析時,本研究發現在south(甲仙區域)的地震群,Vp/Vs值與前人的結果十分相似,也暗示了新方法在台灣地區的可行性。與此同時,east2(花蓮外海區域)的結果則有明顯不同,我們推測原因可能是兩個方法本身解析程度上就有差異,地下構造中流體、裂隙與不同的岩相等相對微小的變化,可能無法被傳統的震波層析成像所解析。另一方面,未來我們可以收集大量的相似波形資料,並配合本研究的資料處理流程,來計算台灣不同地區的Vp/Vs資料,以提供後續的研究使用。 | zh_TW |
dc.description.abstract | In general, variations in Vp/Vs ratios may be determined by using tomographic methods. However, the resolution of local Vp/Vs ratios from tomography is usually limited due to the coarse grid sizes and the regularization operation. Lin and Shearer (2007) proposed that the Vp/Vs ratios could also be estimated within similar earthquake clusters from measuring the P and S differential arrival times with waveform cross-correlation. This technique potentially has higher resolution than typical tomographic inversion method. Benefited by the dense seismic network and high seismicity, Taiwan region is very suitable place for applying this approach to determine Vp/Vs. But the complexity of the geological structure in Taiwan is very different from the Southern California. To consider the effect of different parameter and factor on this new method, synthetic test is used on the similar earthquake cluster in Taiwan region to examine this approach. Also, a robust misfit function method is modified from the previous study to compute Vp/Vs ratios for both synthetic datasets and similar earthquake clusters. In comparison with the results from the latest tomographic model, Vp/Vs ratio of one cluster(Jiaxian area) is very consistent with our result. On the other hand, Vp/Vs ratio of another cluster(Hualian area) is very different from tomographic model. It may indicate the different resolution between two methods, in which, conventional tomographic method may not be able to resolve small scale of heterogeneity. Furthermore, data processing in this study may be used to estimate Vp/Vs ratio for further study or future work in different area. | en |
dc.description.provenance | Made available in DSpace on 2021-06-16T06:41:17Z (GMT). No. of bitstreams: 1 ntu-103-R01224202-1.pdf: 7158010 bytes, checksum: 16b0a26eb99df37212cf1f177ec8724d (MD5) Previous issue date: 2014 | en |
dc.description.tableofcontents | 口試委員會審定書 i
誌謝 ii 摘要 iii Abstract iv 目錄……………………………………………………………………………………v 圖目錄 vii 表目錄 ix 第一章 緒論 1 第二章 文獻回顧 3 2.1 Vp/Vs的定義與柏松比 3 2.2 岩石中的Vp/Vs 4 2.3 Vp/Vs的計算方法 7 第三章 研究方法 9 3.1研究流程簡介 9 3.2理論與假設 10 3.3迴歸方法 15 3.3.1拔靴法 15 3.3.2 P波與S波的資料量值誤差 16 3.3.3迭代式加權最小平方法 16 3.3.4格點搜尋方法 16 3.3.5 迴歸測試 18 3.3 人工測試 21 3.5資料來源與處理 35 3.5.1重覆地震與相似地震目錄 35 3.5.2 資料處理流程 37 3.5.3 使用的地震波形資料 42 第四章 結果與討論 43 4.1 P波與S波的初射角的差異 43 4.2 與震波層析成像的結果比較 43 4.3 地震定位的誤差 44 第五章 結論 47 參考文獻 48 附錄A 54 附錄B 56 | |
dc.language.iso | zh-TW | |
dc.title | 利用相似地震群計算Vp/Vs值運用在臺灣地區 | zh_TW |
dc.title | Estimating Local Vp/Vs ratios within Similar Earthquake Clusters in Taiwan Region | en |
dc.type | Thesis | |
dc.date.schoolyear | 102-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 曾泰琳(Tai-Lin Tseng),郭陳澔(Kuo-Chen Hao) | |
dc.subject.keyword | 台灣,Vp/Vs值,差分時間,相似地震群,波形交叉相關法, | zh_TW |
dc.subject.keyword | Taiwan,Vp/Vs ratios,differential times,similar earthquake clusters,waveform cross-correlation, | en |
dc.relation.page | 61 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2014-07-30 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 地質科學研究所 | zh_TW |
顯示於系所單位: | 地質科學系 |
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