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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 宋國士 | |
dc.contributor.author | Ching-Yu Hu | en |
dc.contributor.author | 胡靚妤 | zh_TW |
dc.date.accessioned | 2021-06-08T03:37:53Z | - |
dc.date.copyright | 2019-07-23 | |
dc.date.issued | 2019 | |
dc.date.submitted | 2019-07-19 | |
dc.identifier.citation | Ben, D. P.& Stephen M.,(2004). Earth Structure [Adobe Digital Editions version]. (Retrieved from http://www.geokniga.org/bookfiles/geokniga-es2e-ch18.pdf)
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Marine Geophysical Researches, 25(1-2), 109-122. 何春蓀. (1975). 臺灣地質概論: 臺灣地質圖說明書. 中華民國經濟部. 許文立.(2001).彰化斷層及其附近構造. 中央大學博士論文. 黃旭燦.(2004). 臺灣中南部褶皺逆衝斷層帶地質構造特徵分析. 中央大學博士論文, 共, 131. 楊耿明.(2002).臺灣西部平原和麓山帶的構造地質.臺灣之活動斷層與地震災害研討會,臺北,143-153 宋國士.(2006). 台中大甲斷層帶西側海域之海陸構造線延伸之海床測繪調 查,國科會期末報告 宋國士.(2017).台灣造山帶的變形前緣(4).台中外海,國科會期末報告 Seismological Laboatory,Department of Geosciences National Taiwan University(http://seismology.gl.ntu.edu.tw/download.htm) 中央地質調查所(https://www.moeacgs.gov.tw/main.jsp) | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/21558 | - |
dc.description.abstract | 臺灣的造山運動,係因菲律賓海板塊與歐亞大陸板塊之間的碰撞作用而引起,以變形前緣做為地質區塊的分界,也是應變作用的交界,在變形前緣以西沒有顯著的地層變形,而變形前緣以東是剛發育的褶皺逆衝帶。
在臺灣造山帶與中國被動大陸邊緣之間的過渡帶在壓應力的作用下產生褶皺逆衝帶,同時發育年輕的斷層與斷層相關褶皺。在褶皺逆衝帶發育的斷層與斷層相關褶皺多為表皮構造,代表在淺部地層發育,並未深入的基盤而是在滑脫面之上。 在前人的研究中,有許多描述臺灣西部與西南部因造山運動而岩石圈側向聚合應變的構造特徵,顯少聚焦在鄰近變形前緣的表皮構造,宋國士(2017)研究中顯示臺中-彰化外海有受到擠壓應力所形成的海底臺地,同時觀察到一系列的構造線型,此處即為褶皺逆衝帶。在上述褶皺逆衝帶發育的岩層條件中,可推測對應力的累積較不易,因此地震活動規模不會太大(M < 5),如在宋國士(2017)的研究中,其研究區域內自1900 年以來芮氏規模大於5 的地震僅有一個事件。 本研究延續宋國士(2017)的研究,透過電花波源和海底地形資料,結合震源機制,以觀察中彰外海之淺層構造特徵及地震活動機制,並探討區域應力的作用與沿岸平臺形成的成因。 | zh_TW |
dc.description.abstract | The collision of Philippine Sea plate and Eurasian Plate formed Taiwan orogen and caused development of fold-thrust belt. At this tectonic setting, it attracted researchers to study about the tectonic patterns and mechanisms in this area. Thus, there are lots of prior studies about tectonic patterns in western and southwestern Taiwan offshore, but few studies focus on the surface structure, especially in Taichung Changhua offshore area.
It’s obviously to find the plateau along the coastline from the topography in study area, and there are a series of structural lineation beneath the plateau, from seismic profiles, and here is so-called fault-thrust belt. Décollement usually develop in the high porosity and moisture weak layer, shale and evaporate for instance, which means that the strata is unable for endure the accumulation of elastic strain for generating greater earthquake. Analyzing earthquake event data from Central Weather Bureau of Taiwan from 1900 till nowadays, there has only one event with M > 5. In this study, we use seismic reflection profiles from sparker and bathymetry data, and analyze focal mechanism from seismic data, to reveal the surface tectonic features and figure out relationship between these tectonic and seismic events. | en |
dc.description.provenance | Made available in DSpace on 2021-06-08T03:37:53Z (GMT). No. of bitstreams: 1 ntu-108-R05241315-1.pdf: 9807444 bytes, checksum: eb5b529c969fddde3eeae750c694d017 (MD5) Previous issue date: 2019 | en |
dc.description.tableofcontents | 口試委員審定書 i
誌謝 ii 中文摘要 iii ABSTRACT iv 目錄 v 圖目錄 vi 表目錄 ix Chapter 1 緒論 1 1.1 前言 1 1.2 研究區域概況 4 1.3 研究目的與動機 16 Chapter 2 研究方法 18 2.1 淺層震測系統 18 2.2 儀器簡介 21 2.3 資料處理 22 Chapter 3 變形前緣與淺層震測剖面 24 3.1 變形前緣定義與淺層構造特徵 24 3.2 淺層反射震測剖面及解釋 32 Chapter 4 地層構造分析與討論 55 4.1 調查區域與陸地地形構造的對比 55 4.2 研究區域地震事件與震源機制分析 63 Chapter 5 結論與建議 65 參考資料 66 | |
dc.language.iso | zh-TW | |
dc.title | 台中-彰化近海的淺部地層構造 | zh_TW |
dc.title | Shallow seismic structure of the Taichung-Changhua
nearshore area | en |
dc.type | Thesis | |
dc.date.schoolyear | 107-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 李錫堤,張翠玉 | |
dc.subject.keyword | 近岸平臺,反射震測法,火花放電,震源機制解, | zh_TW |
dc.subject.keyword | nearshore plateau,seismic reflection method,spark,focal mechanism, | en |
dc.relation.page | 69 | |
dc.identifier.doi | 10.6342/NTU201901608 | |
dc.rights.note | 未授權 | |
dc.date.accepted | 2019-07-19 | |
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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