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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳文山(Wen-Shan Chen) | |
| dc.contributor.author | Tong-Hin Chan | en |
| dc.contributor.author | 陳彤軒 | zh_TW |
| dc.date.accessioned | 2022-11-23T08:59:03Z | - |
| dc.date.available | 2021-11-03 | |
| dc.date.available | 2022-11-23T08:59:03Z | - |
| dc.date.copyright | 2021-11-03 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2021-10-26 | |
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(1985) Fission-track stability in zircons under geological conditions. Nuclear Tracks, 10, 303-307 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79369 | - |
| dc.description.abstract | 當山脈碰撞抬升時，造山前緣會逐漸下陷，形成前陸盆地。因此海岸山脈的後前陸盆地於上新世以來持續堆積了厚層的造山帶沉積物，這些沉積物記錄了山脈的剝蝕歷史。本研究目的為利用海岸山脈後前陸盆地的沉積物，以核飛跡定年法研究，探討中部脊樑山脈在造山時期地殼抬升的冷卻歷史，以了解脊樑山脈的剝蝕歷史。本研究的樣本採集自鹽寮坑溪(十號橋)，地層為蕃薯寮層和八里灣層，採集砂礫岩層中的變質砂岩礫石和基質的砂岩。蕃薯寮層屬於晚上新世的中-下部深海沖積扇、八里灣層為晚上新世至早更新世深海上部沖積扇，皆來自西側的脊樑山脈。由於前人探討海岸山脈盆地的地溫梯度僅有約14˚C/km，故其核飛跡並不會因深埋作用而被癒合，利用盆地地層中碎屑鋯石和磷灰石的核飛跡年代可以計算脊樑山脈的抬升與剝蝕歷史。 本研究指出蕃薯寮層和八里灣層的磷灰石核飛跡的最年輕峰值介於6.6Ma至2.1Ma，越年輕的地層其核飛跡年代也隨之年輕、而礫石中鋯石核飛跡皆為部份癒合(partial annealing)，代表其源區地層並沒受到超過250度以上的熱事件、砂岩的鋯石核飛跡則有一癒合年代峰值4.9Ma。而利用磷灰石和鋯石的核飛跡年代得知當時有兩種不同冷卻路徑的源區，為源自太魯閣帶及玉里帶，及得出於中期上新世時玉里帶脊樑山脈的冷卻速率約52-60˚C/Ma，到了4-3Ma時玉里帶和太魯閣帶有一明顯的加速冷卻。同時利用磷灰石和鋯石核飛跡可以探討源區的剝蝕岩性，約在3.4Ma時(蕃薯寮層)脊樑山脈開始已經出露(被剝蝕)極低度變質的硬頁岩岩層，約3.3Ma時(八里灣層)開始出露低度變質岩層(板岩)。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T08:59:03Z (GMT). No. of bitstreams: 1 U0001-2510202117193800.pdf: 7900184 bytes, checksum: cf397fc5536c6769917bb71f31f9206f (MD5) Previous issue date: 2021 | en |
| dc.description.tableofcontents | 口試委員會審定書 i 致謝 ii 摘要 iv Abstract v 目錄 vi 圖目錄 viii 表目錄 x 第一章 緒論 1 1-1 前言 1 1-2 區域地質概述 2 1-3 前人研究 4 1-4 研究動機與目的 8 第二章 研究方法 10 2-1 核飛跡定年原理 10 2-1-1 核飛跡的形成 10 2-1-2 核飛跡的癒合作用 11 2-2 核飛跡年代的地質意義 13 2-3 核飛跡年代計算 13 2-3-1 核飛跡年代的計算 13 2-3-2 中子通量的計算 15 2-3-3 標準玻璃的zeta(ζ)值校正 16 2-3-4 年代誤差的計算 17 2-3-5 核飛跡年代測定方式 18 2-4 實驗過程 18 2-4-1 樣本的處理流程 18 2-5 鋯石鈾鉛定年之原理 22 第三章 研究結果 23 3-1 核飛跡定年結果 24 3-2 核飛跡顆粒年代頻譜 29 3-2-1 磷灰石核飛跡定年結果 29 3-2-2 鋯石核飛跡定年結果 34 第四章 討論 39 4-1 源區特性分析 40 4-1-1 磷灰石核飛跡年代討論 40 4-1-2 鋯石核飛跡年代討論 42 4-1-3 源區沉積物變質度探討 44 4-2 鋯石鈾鉛定年 46 4-3 冷卻速率與剝蝕速率 49 4-3-1 冷卻速率 49 4-3-2 剝蝕速率 59 4-4 東部盆地的核飛跡癒合程度 60 4-5 台灣造山演變史 66 第五章 結論 67 參考文獻 68 附錄 74 磷灰石核飛跡定年數據 74 鋯石核飛跡定年數據 95 鋯石鈾鉛定年數據 108 | |
| dc.language.iso | zh-TW | |
| dc.title | 利用水璉礫岩的砂岩與礫石之核飛跡定年研究探討上-更新世脊樑山脈剝蝕歷史 | zh_TW |
| dc.title | Apatite and zircon fission track analyses derived from the Shuilien Conglomerate of the Coastal Range: Implication from the Plio-Pleistocene exhumation history of the Backbone Range | en |
| dc.date.schoolyear | 109-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 黃韶怡(Hsin-Tsai Liu),鍾孫霖(Chih-Yang Tseng),顏君毅 | |
| dc.subject.keyword | 核飛跡定年法,剝蝕歷史,海岸山脈,水璉礫岩, | zh_TW |
| dc.subject.keyword | Fission Track thermochronometry,exhumation history,Coastal Range,Shuilien Conglomerate, | en |
| dc.relation.page | 123 | |
| dc.identifier.doi | 10.6342/NTU202104162 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2021-10-27 | |
| 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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