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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 郭本垣(Ban-Yuan Kuo) | |
| dc.contributor.author | Yi-Wei Lin | en |
| dc.contributor.author | 林逸威 | zh_TW |
| dc.date.accessioned | 2021-06-16T13:24:14Z | - |
| dc.date.available | 2014-07-30 | |
| dc.date.copyright | 2013-07-30 | |
| dc.date.issued | 2013 | |
| dc.date.submitted | 2013-07-24 | |
| dc.identifier.citation | Aki, K., Signal to noise ratio in seismic measurements, Tokai University Press, Tokyo, 1976.
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T., R. J. Rau, and D. Salzberg, Taiwan orogeny: Thin-skinned or lithospheric collision?, Tectonophysics, 274 , 191–220, 1997. Yeh, Y. H., et al., Onshore/offshore wide-angle deep seismic profiling in Taiwan, Terr. Atmos. Oceanic Sci., 9 , 301–316, 1998. Yu, H. S., and L. Y. Chiao, The physiography off southern Taiwan coast: Morphology and its implication for trench-continent convergence, Acta Oceanogr. Taiwanica, 33 , 21–37, 1994. Yu, H. S., and G. S. Song, Oblique convergence between trench-arc system and continent-implications for the formation of the submarine physiography off southern Taiwan, Acta Oceanogr. Taiwanica, 32 , 45–53, 1994. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/62033 | - |
| dc.description.abstract | 沿著馬尼拉海溝, 南中國海盆, 也就是歐亞板塊上的海洋性板塊, 隱沒至菲律賓海板塊底下。馬尼拉海溝北段結束在南台灣, 往東傾的隱沒帶, 因為歐亞板塊大陸性邊緣與呂宋島弧碰撞而無法繼續隱沒, 而形成台灣的造山帶。在南臺灣這個大陸性與海洋性板塊的交界帶, 隱沒的構造因為缺乏外海觀測資料的關係, 尚未完全明朗。在本篇論文, 我們使用了從 2009 年至 2011 年兩期佈放於北呂宋海槽附近的海底地震儀資料, 聯合中央氣象局的即時觀測網資料形成陸聯網, 進行地震重定位。我們選用了規模大於二以上的地震, 重定位過後, 其分佈更與地殼以及隱沒板塊接近。並利用此聯合陸上及海上的資料組進行逆推, 以得到此區域的一維平均速度模型。在重定位以及一維平均速度模型逆推皆使用可將測站置於任意一層的高程修正, 以讓一維平均速度模型收斂。 | zh_TW |
| dc.description.abstract | Along the Manila trench the oceanic part of the Eurasian plate, i.e., the South China Sea (SCS) basin,is subducting eastward under the Philippine Sea plate. The Manila trench terminates in the north offshore southern Taiwan, where the subduction is impeded by the collision between the Luzon arc and the Eurasian continental margin which have built the Taiwan orogeny. The subduction zone structure at the ocean-continent junction south of Taiwan is so far unknown because of the lack of in-situ sampling. We have conducted OBS experiments in this region during 2009-2011, and conbined it with CWBSN as onshore-offshore network. Events with M > 2 were relocated to better delineate the crustal and slab structure. We carried out inversion for Vp. In relocation and 1D model inversion, we used height correction which can put station into any layer of velocity model to converge in 1D model inversion. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-16T13:24:14Z (GMT). No. of bitstreams: 1 ntu-102-R98224212-1.pdf: 13963122 bytes, checksum: f3142ee430368c39de2e5853d8c96500 (MD5) Previous issue date: 2013 | en |
| dc.description.tableofcontents | 誌謝 i
中文摘要 ii 英文摘要 iii 圖目錄 vi 表目錄 xii 第一章 緒論 1 第二章 資料 8 2.1 取得資料 9 2.1.1 測站網 9 2.1.2 目錄 12 2.2 拾取前處理 12 2.3 拾取OBS 到時 12 2.3.1 訊噪比 14 2.3.2 濾波器 14 2.3.3 到時與品質 15 2.4 重新檢視CWBSN 到時 18 第三章研究方法 23 3.1 地震重定位 24 3.2 一維速度模型逆推 26 第四章結果與驗證 29 4.1 地震重定位 29 4.1.1 陸聯網 29 4.1.2 縮減之陸聯網 29 4.2 重定位統計 36 4.2.1 最小站間距 36 4.2.2 最大站間角GAP 37 4.2.3 平均對數本徵值ALE 37 4.2.4 方均根殘差RMS 40 4.2.5 測站殘差 41 4.2.6 Importance 54 4.3 一維速度模型及其驗證 68 第五章結論 73 參考資料 75 附錄 A 1 A.1 TRVDRV 的高程修正, 測站在任一層的波線追跡 A 1 A.1.1 折射波的走時 A 2 A.1.2 直達波的走時 A 4 A.1.3 走時的驗證 A 7 A.1.4 走時對於震央距及震源深度的空間微分 A 7 A.2 重定位加權回歸解 A 10 A.3 奇異值分解 A 12 | |
| dc.language.iso | zh-TW | |
| dc.subject | 陸聯網 | zh_TW |
| dc.subject | 南台灣 | zh_TW |
| dc.subject | 重定位 | zh_TW |
| dc.subject | 一維平均速度模型 | zh_TW |
| dc.subject | 海底地震儀 | zh_TW |
| dc.subject | 呂宋島弧 | zh_TW |
| dc.subject | 隱沒帶 | zh_TW |
| dc.subject | Luzon Arc | en |
| dc.subject | Relocation | en |
| dc.subject | 1D Velocity Model | en |
| dc.subject | Subduction Zone | en |
| dc.subject | South of Taiwan | en |
| dc.subject | Onshore-Offshore Network | en |
| dc.subject | OBS | en |
| dc.subject | Ocean Bottom Seismometer | en |
| dc.title | 利用海底地震儀資料研究南台灣隱沒構造 | zh_TW |
| dc.title | Structure of the subduction zone south of Taiwan constrained by OBS data | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 101-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 洪淑蕙(Shu-Huei Hung) | |
| dc.contributor.oralexamcommittee | 張翠玉(Tsui-Yu Chang),張建興(Chien-Hsin Chang) | |
| dc.subject.keyword | 海底地震儀,陸聯網,南台灣,隱沒帶,呂宋島弧,重定位,一維平均速度模型, | zh_TW |
| dc.subject.keyword | Ocean Bottom Seismometer,OBS,Onshore-Offshore Network,South of Taiwan,Subduction Zone,Luzon Arc,Relocation,1D Velocity Model, | en |
| dc.relation.page | 90 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2013-07-24 | |
| 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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