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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 張翠玉 | |
| dc.contributor.author | Shu-Jung Wang | en |
| dc.contributor.author | 王淑榕 | zh_TW |
| dc.date.accessioned | 2021-05-20T20:32:33Z | - |
| dc.date.available | 2011-08-06 | |
| dc.date.available | 2021-05-20T20:32:33Z | - |
| dc.date.copyright | 2008-08-06 | |
| dc.date.issued | 2008 | |
| dc.date.submitted | 2008-07-30 | |
| dc.identifier.citation | Brown, G.C. & Mussett, A.E. (1993), The Inaccessible Earth : an Integrated View to its Structure and Composition. 2nd ed. Chapman & Hall.
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Sato Toshinori, Sadayuki Koresawa, Yasumasa Shiozu, Fujio Kusano, Seiichi Uechi, Osamu Nagaoka and Junzo Kasahara (1994), Microseismicity of Back-Arc Rifting in the Middle Okinawa Trough, Geophysical Research Letters, 21, NO. 1, 13–16 Shyu, C. T. and C. S. Liu (2001), Heat flow of the southwestern end of the Okinawa Trough, TAO, Supplementary Issue, 305-317. Sibuet, J.-C., B. Deffontaines, S.-K. Hsu, N. Thareau, J.-P. Le Formal, and C.-S. Liu (1998), The southwestern Okinawa Trough back-arc basin: Tectonics and volcanism, J. Geophys. Res., 103, 30245– 30267. Sibuet, J.C., Letouzey, J., Barbier, F., Charvet, J., Fourcher, J.P., Hilde, T.W.S., Kimura, M., Chiao, L.Y., Marsset, B., Mueller, C., Stephen, J.F., 1987. Back-arc extension in the Okinawa Trough. Journal of Geophysical Research, 92 (B13), 14041-14063. Stuart, G.W.; Bastow I.D.; Ebinger C.J. (2006) Crustal structure of the northern Main Ethiopian Rift from receiver function studies, In: G. Yirgu, C. Ebinger and P. 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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/9632 | - |
| dc.description.abstract | 菲律賓板塊以每年8公分-北偏西50度的運動速度，向歐亞大陸相互聚合。 在台灣東北海域，菲律賓板塊隱沒於歐亞大陸板塊之下，受到板塊隱沒-碰撞作用，遂於琉球島弧後方拉張形成南沖繩海槽，海槽內地震活動頻繁，對該地區構造運動動力來源，提供豐富的研究資料。然受限於目前地震測站多位於台灣本島限制，角度覆蓋偏窄的問題使得海槽內的地震定位存在一定的不準確度，因此本研究使用佈置於海槽張裂軸附近的寬頻海底地震儀（Broad-Band Ocean Bottom Seismometer，1站），結合「台灣寬頻地震觀測網」（BATS，7站）及「日本寬頻地震網」（F-net，2站）所收錄之寬頻地震儀記錄資料，標定地震的震源參數，以提供當地地震分佈及速度模式更好的解析。
本研究以地震定位之走時殘差值，進行一維速度模式逆推，建立南沖繩海槽全區域的速度模式，並依此速度模式將地震重新定位，而後利用雙差分地震定位法，修正地震的空間分佈，得到地震對之間相對準確的地震位置。下一步則再次篩選出OBS30測站接收分佈於張裂軸附近(北緯24.4~25.1度,東經122.7~123.6度,深度0~50km)的波相到時，針對南沖繩海槽張裂軸速度模式進行逆推。希望能透過速度模型的討論，對南沖繩海槽地殼構造特性，有更多的了解。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-05-20T20:32:33Z (GMT). No. of bitstreams: 1 ntu-97-R95241314-1.pdf: 3703480 bytes, checksum: 94ed260d788b67b3ce45e7010d203bc2 (MD5) Previous issue date: 2008 | en |
| dc.description.tableofcontents | 摘要 I
致謝 II 目錄 III 圖目錄 V 表目錄 VII 第一章 緒論 1 1-1 研究區域概況 1 1-2 研究動機與目的 5 1-3 本文內容 6 第二章 地震記錄與資料處理 8 2-1 地震資料來源 8 2-2 地震資料處理流程 8 2-2-1 地震事件挑選方法 12 2-2-2 定位程式 - SEISAN初始參數設定 13 2-2-3 定位判定原則與結果 18 2-3 初步地震定位結果 18 第三章 一維速度模式逆推 22 3-1 基本原理 22 3-2 資料選取與參數設定 25 3-3 不同初始速度模型的比較 28 第四章 地震重新定位 36 4-1 全區域速度模式地震定位結果 36 4-2 雙差分地震定位法 36 4-2-1 基本原理 36 4-2-2 雙差分定位法重新定位結果 38 4-3 地震空間分布與當地構造的對應 38 第五章 討論與結論 45 5-1 全區域一維速度模式與板塊物理性質 45 5-2 張裂軸一維速度模式與板塊物理性質 45 附錄A OBS計畫之寬頻海底地震儀系統簡介 52 附錄B BATS簡介 59 附錄C F-net簡介 60 參考文獻 61 | |
| dc.language.iso | zh-TW | |
| dc.title | 南沖繩海槽之地殼構造 | zh_TW |
| dc.title | The Crustal Structure of Sourthern Okinawa Trough | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 96-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 喬凌雲 | |
| dc.contributor.oralexamcommittee | 郭本垣,洪淑蕙 | |
| dc.subject.keyword | 沖繩海槽,雙差分,海底寬頻地震儀, | zh_TW |
| dc.subject.keyword | Okinawa Trough,Double difference,OBS, | en |
| dc.relation.page | 65 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2008-07-31 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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