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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 徐澔德(J. Bruce H. Shyu),李建成(Jian-Cheng Lee) | |
| dc.contributor.author | Yu Wu | en |
| dc.contributor.author | 吳俁 | zh_TW |
| dc.date.accessioned | 2021-06-08T02:41:05Z | - |
| dc.date.copyright | 2018-03-01 | |
| dc.date.issued | 2018 | |
| dc.date.submitted | 2018-02-13 | |
| dc.identifier.citation | References
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He (2009), “Uniform geothermal gradient” and heat flow in the Qiongdongnan and Pearl River Mouth Basins of the South China Sea, Marine and Petroleum Geology, 26(7), 1152-1162, doi: https://doi.org/10.1016/j.marpetgeo.2008.08.008. 中文參考文獻 何春蓀（1975）臺灣地質概論─臺灣地質圖說明書。經濟部中央地質調查所出版，共117頁。 何春蓀（1986）臺灣地質概論─臺灣地質圖說明書，增訂第二版。經濟部中央地質調查所出版，共163頁。 李彥良、李錦發、梁均合（2008）眉溪砂岩分布與特性探討。經濟部中央地質調查所96年度業務成果發表會手冊，第39頁。 林啟文、劉桓吉、林偉雄、羅偉、高銘健（2008）雪山山脈白冷層的層位與構造探討。2008台灣構造地質研討會大會手冊及論文集，第7-11頁。 陳勉銘、游能悌、朱傚祖、謝凱旋、謝有忠（2009）雪山山脈南段武界地區所謂「眉溪砂岩」發現的古第三紀大型有孔蟲露頭。經濟部中央地質調查所特刊，第22號，第227-242頁。 陳肇夏（1992）台灣雪山山脈與中央山脈第三紀地層的對比問題。經濟部中央地質調查所特刊，第6號，第39-68頁。 陳肇夏、王京新（1995）臺灣變質相圖說明（第二版）。經濟部中央地質調查所特刊，第2號，共51頁。 曹恕中（1996）臺灣中央山脈變質沉積岩伊萊石結晶度、鋯石核飛跡年代和鉀氬年代之地質意義。國立臺灣大學地質研究所博士論文，共272頁。 黃鑑水、李錦發（1992）雪山山脈眉溪砂岩之地層沈積環境及其與四稜砂岩之關係。經濟部中央地質調查所特刊，第6號，第143-152頁。 黃鑑水、陳勉銘、謝凱旋（2000）埔里圖幅及說明書。五萬分之一台灣地質圖，第三十二號，經濟部中央地質調查所出版，共75頁。 劉桓吉（1997）臺灣雪山山脈中部之地質構造與地層研究。國立臺灣大學地質學研究所博士論文，共113頁。 劉桓吉、楊昭男（1992）臺灣雪山山脈濁水溪之地質。經濟部中央地質調查所彙刊，第8號，第31-61頁。 劉桓吉、高銘健（2010）梨山地質圖幅及說明書，臺灣五萬分之一地質圖幅第十九號。經濟部中央地質調查所出版，共73頁。 謝凱旋（2009）雪山山脈的生物地層對比探討。經濟部中央地質調查所特刊，第22號，第13-45頁。 謝凱旋、洪崇勝、陳勉銘、游能悌（2011）臺灣中部地區佳陽層、眉溪砂岩中段與廬山層底部之化石研究：雪山山脈南段東翼地層的年代制約。經濟部中央地質調查所特刊，第25號，第133-166頁。 羅偉、楊昭男（2002）霧社地質圖幅及說明書，臺灣五萬分之一地質圖幅第二十六號。經濟部中央地質調查所出版，共59頁。 羅偉、吳樂群、陳華玟（1999）國姓地質圖幅及說明書，臺灣五萬分之一地質圖幅第二十五號。經濟部中央地質調查所出版，共71頁。 經濟部中央地質調查所（2000）臺灣地質圖(1:500,000)，新北市：經濟部中央地質調查所出版。 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/20155 | - |
| dc.description.abstract | 台灣造山帶是由呂宋島弧碰撞歐亞板塊被動大陸邊緣所形成，此一典型造山帶地表出露之岩石大部分是由被動大陸邊緣基盤及其上沉積物堆疊變形而成。其中，雪山山脈原為始新世至中新世時被動大陸邊緣半地塹中的沉積物，於碰撞造山後加入造山楔中，成為現今的雪山山脈。若能了解雪山山脈的變質溫度紀錄，進一步推演物質之熱運動學歷史，對重建台灣造山帶的演化過程有很大的幫助。而一直以來都具有爭議的雪山山脈─脊梁山脈板岩帶邊界的性質，也能透過邊界兩側之變質溫度分布來判明。
因板岩帶地層中多富含碳質物，本研究將以碳質物拉曼光譜法(Raman spectroscopy of carbonaceous material, RSCM)來測量岩石在深埋及抬升變形中所經歷過的最高溫度(maximum temperature, TM)，於本研究中稱為RSCM-T。 本研究於前人工作資料較少雪山山脈南段及其相鄰脊梁山脈板岩帶中，以約2公里的間隔沿著垂直該區域岩層走向的剖面採集25個RSCM樣本，建立兩條橫跨雪山山脈南段與相鄰脊梁山脈板岩帶的RSCM-T剖面。由實驗所得RSCM-T剖面中可觀察出，本研究區域中地利斷層以東的內雪山山脈地層中所測得之RSCM-T皆相當接近，指示了內雪山山脈地層經歷了「褶皺後達到最高溫度」之變形模式；而在脊梁山脈板岩帶中，北、中、南段皆有RSCM-T向東增加之趨勢；此外也確認雪山山脈與脊梁山脈板岩帶之間應存在梨山斷層，將雪山山脈一側抬升；而內雪山山脈中可能還存在一沉積年代為漸新世晚期至中新世早期的板岩層。 分析台灣中部板岩帶熱變質紀錄後，本研究提出了雪山山脈南段之內雪山山脈以及梨山斷層其地層為主之變質、變形歷史，認為內雪山山脈地層先隨著被動大陸邊緣俯衝至造山楔下方，遭基底滑脫面之雙軌構造帶入台灣造山帶底部，並受到褶皺變形，接著被加溫達到TM，最終抬升至現今位置。 | zh_TW |
| dc.description.abstract | Taiwan orogenic belt is built by the collision between the Luzon arc of the Philippine Sea plate and the passive continental margin of the Eurasian plate. Rocks exposed in the orogenic belt were mostly deformed from the passive margin basement and cover series. Among the whole orogeny belt, the slate belt, which contains the Hsuehshan Range (HR) and the Backbone Range slate belt (BRSB), is composed of metamorphosed Eocene to Miocene sediments which experienced only the Neogene Taiwan orogeny after diagenesis at the passive margin. Characterizing the thermal metamorphic history of the slate belt is essential for reconstructing its geological evolution during the mountain building processes. The so far controversial contact relationship between HR and its juxtaposed BRSB can also be resolved by the thermal metamorphic documentation.
Since carbonaceous material is common in pelitic protolith of slates in the slate belt, the Raman spectrum of carbonaceous material (RSCM) measuring the rock maximum temperature(TM) is chosen for quantitative thermal metamorphic documentation. TM which measured from RSCM method is called RSCM-T in this research. Previous studies have mostly focused on northern and central part of HR and presented different thermal metamorphic histories. Therefore, the target of this study is to obtain and analyze the thermal metamorphic documentation in the southern part of HR and the juxtaposed BRSB. 25 samples are taken from the Puli and Wushe area in Central Taiwan slate belt with a dense 2-km spacing, and two maximum temperature profiles are constructed. Results show that protolith of inner HR, which located on the eastern side of the Tili fault, had been folded while it reached maximum heating stage, and the eastward increasing trend of RSCM-T is found in the juxtaposed BRSB. Furthermore, the existence of Lishan Fault, which made its western side uplifted, is confirmed at the boundary between HR and BRSB. Furthermore, a slate formation which deposited in late Oligocene to early Miocene is proposed to be the youngest layer in the inner HR. The evolution history of inner HR and Lishan Fault inferred from the result shows that the proto-inner HR strata were deformed and transferred from the passive margin into orogenic wedge through the basal accretion mechanism, and then achieved maximum heating. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-08T02:41:05Z (GMT). No. of bitstreams: 1 ntu-107-R04224208-1.pdf: 7608713 bytes, checksum: 07af857789ae996e331a3dd248deef9a (MD5) Previous issue date: 2018 | en |
| dc.description.tableofcontents | 口試委員審定書 I
誌謝 II 中文摘要 IV Abstract V 圖目錄 IX 表目錄 XI 第1章、 前言 1 第2章、 地質背景 4 2.1. 雪山山脈及脊梁山脈板岩帶之地層與構造 4 2.1.1. 雪山山脈地質區 4 2.1.2. 脊梁山脈板岩帶地質區 7 2.1.3. 板岩帶的地層對比 8 2.1.4. 板岩帶地層原始沉積架構 9 2.1.5. 雪山山脈─脊梁山脈板岩帶邊界之意義 10 2.2. 造山帶變質度及熱定年研究 12 2.2.1. 物質加入造山帶之方式 12 2.2.2. 台灣造山帶之形成機制 14 2.2.3. 台灣造山帶中之變質礦物相研究 15 2.2.4. 台灣造山帶中之低溫熱定年研究 18 2.2.5. 台灣造山帶中之熱變質溫度研究 22 第3章、 研究方法 24 3.1. 野外觀察及岩石樣本採集 24 3.2. 熱變質溫度指標：碳質物拉曼光譜 26 3.2.1. 碳質物的特性 26 3.2.2. 碳質物拉曼光譜的組成及特徵 26 3.2.3. 碳質物拉曼光譜的應用 28 3.2.4. 樣本製備 30 3.2.5. 碳質物拉曼光譜的測量 32 第4章、 研究結果 34 4.1. 採樣點位置 34 4.2. 拉曼光譜分析結果 38 4.3. 雪山山脈南段及相鄰脊梁山脈板岩帶之最大變質溫度分布 40 4.3.1. 地利斷層兩側之RSCM-T分布特徵 40 4.3.2. HBB兩側之RSCM-T分布特徵 41 4.3.3. 內雪山山脈之RSCM-T分布特徵 41 4.3.4. 外雪山山脈之RSCM-T分布特徵 42 4.3.5. 脊梁山脈板岩帶之RSCM-T分布特徵 42 第5章、 討論 45 5.1. 內雪山山脈RSCM-T分布指示之變形模式 45 5.1.1. 被動大陸邊緣地層─溫度架構 45 5.1.2. 雪山山脈南段之內雪山山脈RSCM-T分布與變形歷史之指示 46 5.1.3. 雪山山脈中段之內雪山山脈RSCM-T分布與變形歷史之指示 48 5.1.4. 雪山山脈北段之RSCM-T分布與變形歷史之指示 50 5.1.5. 雪山山脈北、中、南段變形模式之小結 52 5.2. HBB之性質及位置探討 53 5.2.1. 由RSCM-T分布推論斷層之存在 53 5.2.2. 梨山斷層之存在及性質探討 55 5.2.3. 梨山斷層之位置討論 58 5.2.4. 內雪山山脈漸新世至中新世板岩層之界定 62 5.3. 脊梁山脈板岩帶變質溫度之指示 65 5.4. 本研究區域之RSCM-T分布於台灣造山帶演化歷史之指示 68 第6章、 結論 70 參考文獻 72 附錄 各樣本拉曼光譜測量結果 79 | |
| dc.language.iso | zh-TW | |
| dc.title | 從台灣中部板岩帶之熱變質記錄探討台灣活動造山帶構造演化 | zh_TW |
| dc.title | Structural evolution of active Taiwan orogeny inferred from thermal metamorphic documentation of central Taiwan slate belt | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 106-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 朱傚祖(Hao-Tsu Chu),詹瑜璋(Yu-Chang Chan),陳致同(Chih-Tung Chen) | |
| dc.subject.keyword | 台灣造山帶,雪山山脈,梨山斷層,變質溫度,碳質物拉曼光譜(RSCM), | zh_TW |
| dc.subject.keyword | Taiwan orogeny,Hsuehshan Range,Lishan fault,thermal metamorphism,Raman spectrum of carbonaceous material (RSCM), | en |
| dc.relation.page | 103 | |
| dc.identifier.doi | 10.6342/NTU201800497 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2018-02-13 | |
| 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 | |
文件中的檔案：
| 檔案 | 大小 | 格式 | |
|---|---|---|---|
| ntu-107-1.pdf 未授權公開取用 | 7.43 MB | Adobe PDF |
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