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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳文山 | |
| dc.contributor.author | Shih-Jie Syu | en |
| dc.contributor.author | 徐士捷 | zh_TW |
| dc.date.accessioned | 2021-06-17T02:44:37Z | - |
| dc.date.available | 2022-08-30 | |
| dc.date.copyright | 2017-08-30 | |
| dc.date.issued | 2017 | |
| dc.date.submitted | 2017-08-15 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/68966 | - |
| dc.description.abstract | 當造山山脈隆起同時，造山前緣逐漸下陷形成前陸盆地，因此前陸盆地沉積物隨晚中新世以來的造山運動，紀錄了剝蝕來自山脈沉積物的演變。本研究利用砂岩岩象（粗砂）與單晶質石英顆粒的圓度分析，探討晚中新世以後砂岩組成變化與中南部造山山脈的剝蝕歷史。從臺灣造山山脈出露的岩層層序來看，剝蝕層序依序應從未膠結的沉積層開始，之後陸續出露成岩相的沉積岩層（中新統砂岩與頁岩），葡萄石-綠纖石相的極低度變質岩（中新統至始新統的變質砂岩與硬頁岩），綠色片岩相的低度變質岩（中新統至始新統的石英岩與板岩）。以下為南部一個地區的岩象分析與單晶質石英顆粒的圓度分析結果。
中部地區濁水溪以南顯示（1）上新世早期之前＞4 Ma（大窩砂岩下部），岩性以大量單晶質石英為主，少量的岩屑則以片岩為主；（2）上新世晚期約4-2.6 Ma（上部大窩砂岩至錦水頁岩）出現少量沉積岩岩屑（1-2%），且隨時代愈年輕至更新世早期2.6-2.0 Ma（卓蘭層下部），沉積岩岩屑逐漸變多（6-20%），片岩岩屑隨著逐漸變少；（3）更新世早期約2.0 Ma（卓蘭層中部）開始出現硬頁岩以及極低度變質砂岩岩屑（2-15%）；（4）更新世早期約1.5 Ma（頭嵙山層底部）則開始大量出現板岩以及低度變質砂岩岩屑（20%）。 單晶質石英顆粒的圓度分析目的為探討造山最初期的未膠結沉積物出露時代，本研究結果顯示最佳圓度變化出現在晚中新世約5.5 Ma（關刀山砂岩上部），而晚上新世約4 Ma（大窩砂岩上部）之後開始圓度變差，且同時岩象顯示沉積岩岩屑開始出現。上述結果得知單晶質石英的圓度變佳的原因，推測是因為來自沉積岩層上覆未膠結的沉積層被侵蝕搬運再度磨圓導致，而沉積岩岩屑的出現則造成圓度開始變差。 對比上述岩象與單晶質石英顆粒的圓度分析結果，顯示沉積物來源由被動式大陸邊緣轉變成造山帶的過渡帶變化可能位在晚中新世，且山脈呈現一反剝蝕現象。 高屏地區以及東部地區在上新世早期至晚期已經接收到板岩岩屑，為侵蝕來自於中新世中期至晚期隱沒作用產生的變質混同層（玉里帶）。台中地區以北的前陸盆地在更新世晚期開始接收到板岩岩屑，濁水溪以南地區在更新世早期開始接收到板岩岩屑，是由於雪山山脈不同區塊有不同的冷卻歷史以及古河系發育規模不同所造成，造成不同的河川沉積系統出現不同的沉積遲滯時間。 彙整造山帶前人的低溫熱定年資料，得知造山帶各區塊的冷卻歷史、岩性出露歷史以及斷層可能的活動時間，並配合沉積盆地砂岩岩象結果得知前陸盆地來源演化與造山帶剝蝕間的沉積物源－滙關係。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-17T02:44:37Z (GMT). No. of bitstreams: 1 ntu-106-R03224112-1.pdf: 15658143 bytes, checksum: a1c4ee6abb3cb9a34e0f99045d352757 (MD5) Previous issue date: 2017 | en |
| dc.description.tableofcontents | 口試委員審定書 I
致謝 II 摘要 IV 目錄 VI 圖目錄 IX 表目錄 XII 第一章 緒論 1 1.1 前言 1 1.2 前人研究 2 1.3 研究動機與目的 3 第二章 區域地質概況 8 2.1 研究區域 8 2.2 岩石地層概述（晚中新世至更新世） 11 2.2.1 中部西部麓山帶岩石地層 11 2.2.2 南部西部麓山帶岩石地層 14 2.2.2.1 曾文溪以北流域（崙後段層以西） 14 2.2.2.2 曾文溪以東流域（崙後段層與平溪段層以東） 17 2.2.2.3 曾文溪以南流域（左鎮斷層以南區域） 20 2.2.3 海岸山脈地層概述 24 第三章 研究方法 26 3.1 岩象分析方法 26 3.1.1 臺灣造山帶來源區地層岩象特徵 27 3.1.2 岩象分析 35 3.1.3 岩象學特徵組合 40 3.2 顆粒形態分析（應用於單晶質石英顆粒） 41 3.2.1 ImageJ（IJ）軟體進行顆粒測量與計算方法 42 3.2.1.1 ImageJ（IJ）三種圓度計算與鮑爾斯的圓度劃分等級對比 44 3.3 低封存溫度熱定年應用 46 3.3.1 整合各熱定年溫度計應用於地殼抬升冷卻歷史 48 第四章 結果 52 4.1 砂岩岩象分析結果 52 4.1.1 中部麓山帶 52 4.1.2 西南部麓山帶 59 4.1.2.1 曾文溪以北流域（崙後斷層以西） 59 4.1.2.2 曾文溪以南流域（左鎮斷層以南區域） 68 4.1.2.3 六龜礫岩 73 4.1.3 海岸山脈 76 4.2 單晶質石英顆粒圓度分析結果 81 第五章 討論 86 5.1 造山帶斷層發育以及剝蝕歷史 86 5.1.1 中部西部麓山帶斷層活動歷史 86 5.1.1.1 中部中央山脈冷卻歷史 88 5.1.2 南部麓山帶斷層活動歷史 91 5.1.2.1 南部造山帶抬升歷史以及剝蝕歷史 94 5.2 前陸盆地來源演化與造山帶剝蝕間的沉積物源－滙關係 101 5.2.1 中部地區（濁水溪以南）前陸盆地沉積物的源－滙系統分析 101 5.2.2 嘉南地區前陸盆地沉積物的源－滙系統分析 104 5.2.3 高屏地區前陸盆地沉積物的源－滙系統分析 109 5.2.4 東部地區碰撞盆地沉積物的源－滙系統分析 112 5.3 綜合討論 115 第六章 結論 119 參考文獻 120 附錄 129 | |
| dc.language.iso | zh-TW | |
| dc.title | 晚中新世以來沉積岩岩象分析探討臺灣南部山脈剝蝕歷史 | zh_TW |
| dc.title | Petrographic study of the Miocene-Pleistocene sandstones in the Western Foothills, southern Taiwan: implication for the unroofing history of Taiwan orogenic belt | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 105-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 吳樂群,游能惕,楊志成 | |
| dc.subject.keyword | 岩象學,前陸盆地,源匯關係,造山帶, | zh_TW |
| dc.subject.keyword | petrography,foreland basin,source-to-sink system analysis,mountain belt, | en |
| dc.relation.page | 139 | |
| dc.identifier.doi | 10.6342/NTU201703222 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2017-08-16 | |
| 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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