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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 宋聖榮(Sheng-Rong Song) | |
| dc.contributor.author | Pei-Chu Chen | en |
| dc.contributor.author | 陳佩竹 | zh_TW |
| dc.date.accessioned | 2021-06-08T05:15:38Z | - |
| dc.date.copyright | 2011-08-04 | |
| dc.date.issued | 2011 | |
| dc.date.submitted | 2011-07-30 | |
| dc.identifier.citation | Bailey, S. W. (1966). The Status of Clay Mineral Structures. 14th National Conference on Clays and Clays Minerals, New York: pergamon.
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Hower (1963). 'Petrological Significance of Illite Polymorphism in Paleozoic Sedimintary Rocks.' American Mineralogist 48(11-2): 1239-1254. Venkataraman, A. and H. Kanamori (2004). 'Observational constraints on the fracture energy of subduction zone earthquakes.' Journal of Geophysical Research-Solid Earth 109(B5). Wilson, B., T. Dewers, Z. Reches and J. Brune (2005). 'Particle size and energetics of gouge from earthquake rupture zones.' Nature 434(7034): 749-752. Yu, S. B., H. Y. Chen and L. C. Kuo (1997). 'Velocity field of GPS stations in the Taiwan area.' Tectonophysics 274(1-3): 41-59. 何信昌、陳勉銘 (2000). 五萬分之一臺灣地質圖說明書圖幅第24號-臺中, 經濟部中央地質調查所. 何春蓀 (1986). 臺灣地質概論: 臺灣地質圖說明書(增訂第二版). 臺北縣, 經濟部中央地質調查所出版. 宋聖榮、王珮玲、鄧茂華、陳于高、陳文山、楊燦堯、李元希、李德貴、詹瑜璋、李建成 (2004)，台灣車籠埔鑽井岩芯和流體的物理、化學性質和微生物，行政院國家科學委員會專題研究計畫成果報告，計畫編號：NSC 93-2119-M-002-028 李麗君 (2003). 奈米石英之合成研究. 地質科學研究所. 臺北市, 國立臺灣大學. PhD: 172. 游艾琦 (2008). 臺灣車籠埔斷層鑽探計劃A井岩心之破裂能研究. 地質科學研究所. 臺北市, 國立臺灣大學. Master: 86. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/24087 | - |
| dc.description.abstract | Analyzing the particle size, shape and orientation on the faulting material has become a routine but important work in the fault zone. These data provide characteristics of fragmentation and comminuting process, and go further for information of fracture energy. In order to calculate the fracture energy, we need to know the particle size distributions of fault gouge which determine total fracture surface area. However, the finest particle of gouge or threshold of lower cut-off particle size is the most important parameter to dominate the amount of surface area. For example, there were different lower cut-off particle sizes in the Punchbowl and Chelungpu faults, with 1.6 nm and 50 nm respectively. Criteria for determining the threshold of lower cut-off size in the Chelungpu fault is the main purpose in this study.
For comparing the mineral assemblage and the finest particles, we collected the samples from wall rock, fault damage zone, and fault core. Then, using the wet sieving, sedimentation, ultracentrifugation and automated ultrafiltration device (AUD) we separated the sizes of particle. Furthermore, particles in different size ranges (whole, 450-2000nm, 100-450nm, 50-100nm, < 50nm) and mineralogy were analyzed by the SEM, TEM and Synchrotron XRD. The wall rock from Chelungpu fault zone consists predominantly of quartz, chlorite, feldspar, kaolinite and 2M1-illite with the minimum particle size ranging from 50 to 100 nm. The results infer that the finest particle in natural sedimentary grinding is around 50 nm in diameter. In the other words, the fault core has the same mineral assemblage as wall rock, but the particle is finer than 50 nm, which comminuted by faulting. Based on the images of TEM, diameter of finest particle can be measured as, 29nm in average. Accordingly, this study calculates the fracture energy of 1999 Taiwan Chi-Chi earthquake as 6.04 MJm-2. Furthermore, the radiation efficiency is 0.83 that shows Chelungpu fault is a mature fault and the energy will be released with the radiation energy rather than the fracture energy during faulting. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-08T05:15:38Z (GMT). No. of bitstreams: 1 ntu-100-R98224202-1.pdf: 19791594 bytes, checksum: 7be69b2cee0d4d61e0cba629e6534055 (MD5) Previous issue date: 2011 | en |
| dc.description.tableofcontents | 口試委員會審定書
誌謝 i 中文摘要 ii ABSTRACT iii 目錄 v 圖目 viii 表目 xii 第一章 緒論 1 1.1 前言 1 1.2 前人研究 2 1.2.1 破裂能 2 1.2.2 輻射效率(radiation efficiency) 4 1.2.3 礦物顆粒大小分布 5 1.3 研究目的 6 第二章 地質概述 7 2.1 區域地質 7 2.2 地層 8 2.3 車籠埔斷層 9 2.4 臺灣車籠埔斷層深鑽計畫 9 第三章 實驗流程與研究方法 11 3.1 實驗材料 12 3.2 實驗儀器 15 3.2.1 高速離心機Hitachi CR21 15 3.2.2 高效率收集奈米粒子儀 17 3.2.3 場發射掃描式電子顯微鏡(SEM) 18 3.2.4 穿透式電子顯微鏡(TEM) 19 3.2.5 同步輻射X光粉末繞射儀(XRD) 20 3.2.6 冷凍乾燥機 22 3.3 數據分析 23 3.3.1 計算奈米級顆粒平均粒徑 23 3.3.2 破裂能計算方法 24 3.3.3 伊萊石同質異型(polytype)分析 25 第四章 研究結果 27 4.1 X光粉末繞射儀分析結果 27 4.1.1 圍岩 29 4.1.2 破裂帶 35 4.1.3 斷層核心 43 4.2 場發射掃描式電子顯微鏡 51 4.3 穿透式電子顯微鏡 52 4.3.1 圍岩 53 4.3.2 破裂帶 53 4.3.3 斷層核心 54 4.3.4 斷層核心破裂能計算 57 第五章 討論 59 5.1 實驗方法探討 59 5.2 沉積環境礦物相與圍岩樣本比較 60 5.3 斷層帶礦物相之顆粒大小及外型討論 62 5.4 主要滑動帶破裂能計算及輻射效率的探討 64 第六章 結論 66 參考文獻 67 附錄一 穿透式電子顯微鏡影像，斷層核心樣本，深度1136.35公尺 72 | |
| dc.language.iso | zh-TW | |
| dc.subject | 車籠埔斷層 | zh_TW |
| dc.subject | 顆粒大小 | zh_TW |
| dc.subject | 破裂能 | zh_TW |
| dc.subject | 輻射效率 | zh_TW |
| dc.subject | 車籠埔斷層深鑽計劃 | zh_TW |
| dc.subject | Fracture energy | en |
| dc.subject | Particle size | en |
| dc.subject | Chelungpu fault | en |
| dc.subject | Taiwan Chelungpu-fault Drilling Project | en |
| dc.subject | radiation efficiency | en |
| dc.title | 臺灣車籠埔斷層帶計算破裂能之最小顆粒 | zh_TW |
| dc.title | The Finest Particle for Calculating Fracture Energy of Taiwan Chi-Chi Earthquake | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 99-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 洪日豪,葉恩肇,陳惠芬 | |
| dc.subject.keyword | 車籠埔斷層,顆粒大小,破裂能,輻射效率,車籠埔斷層深鑽計劃, | zh_TW |
| dc.subject.keyword | Chelungpu fault,Particle size,Fracture energy,radiation efficiency,Taiwan Chelungpu-fault Drilling Project, | en |
| dc.relation.page | 78 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2011-08-01 | |
| 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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