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| ???org.dspace.app.webui.jsptag.ItemTag.dcfield??? | Value | Language |
|---|---|---|
| dc.contributor.advisor | 盧佳遇 | |
| dc.contributor.author | Yi-Chun Hsu | en |
| dc.contributor.author | 徐乙君 | zh_TW |
| dc.date.accessioned | 2021-06-13T15:18:17Z | - |
| dc.date.available | 2008-07-26 | |
| dc.date.copyright | 2008-07-26 | |
| dc.date.issued | 2008 | |
| dc.date.submitted | 2008-07-23 | |
| dc.identifier.citation | 中文部份
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/37042 | - |
| dc.description.abstract | 本研究區位於台灣東南部的太麻里海岸一帶，由於正好處於菲律賓海板塊與歐亞板塊之隱沒-碰撞的過度帶，此處的岩層完整紀錄台灣早期造山階段的特徵和橫移壓縮的過程。本區之岩層以中新世的廬山層為主，由黑色到深灰色的硬頁岩、板岩和深灰色的硬砂岩互層組成，以及複理層沉積物，中間夾有一些透鏡狀砂岩以及散亂的泥球結核；這些地層都經過低度變質其變質度可達葡萄石-綠纖石相，由野外觀察可看出此區已歷經多次的變形作用。
本研究除了藉由野外的觀察與構造測量分析外，尚利用板岩內的壓影構造(pressure shadow)構造重建岩石變形歷史，分析壓影構造首先要將採集的岩層的定向標本，在變質岩韌性剪切帶中，一般認為主要葉理面代表剪動面，主要剪動面即為XY面，而剪動面上的伸張線理方向即為有限應變橢球的最長軸方向，亦即X軸方向；分別由劈理面及伸張線理的方向決定三互相垂直的XY面、XZ面及YZ面，觀察這三面薄片中的壓影纖維構造及層面和劈理面的相關性以進行分析；除此之外，並加上磁感率異向性分析，對金崙類背斜之褶皺進行探討。 從野外的觀測上，可發現此區普遍存在一組呈次水平的劈理(Sh)和一組成東南東方向的線理(L)。而本研究主要分析五個褶皺露頭之次水平劈理上的壓影構造，欲了解其褶皺和劈理的相關性。 分析結果發現：(1) 此區的壓影構造大多是黃鐵礦型態(pyrite type)。仔細觀察薄片上的壓影構造，則發現不論是在XY面上或是在XZ面上甚至是YZ面上都可觀察到非共軸變形，由壓影纖維構造於空間上的分布情形可以推論其形成主要是受控於向東活動的逆衝斷層帶的影響，並記錄到塊體順時針旋轉的現象，且壓影纖維構造於形成之後，仍有受到後期板岩中固定流動(flexural flow)的影響。(2) 由磁感率異向性的分布則可得知於褶皺兩翼的受力情形並不相同，和所觀察到的不對稱褶皺現象相符。(3) 野外的次水平分布的葉理面，以及壓影纖維構造上放射狀的纖維，都可得知此區曾受到垂直方向的壓縮。(4) 從野外觀察到的中視尺度之截切關係加上壓影纖維構造的分析結果可以得知此區的變形歷史。 此結果顯示此區的變形歷史相當複雜，推論其反應出在抬升的階段中，三軸變形和垂直壓縮是主要的變形機制。 | zh_TW |
| dc.description.abstract | Since the geometries of syn-tectonic fibers in pressure shadows are considered to be closely related to the deformation paths of host rocks, syn-tectonic fibers have been used to determine fold kinematics and the kinematics of deformation in accretionary prism and fold-and-thrust belt. This study uses pressure shadows to analyze rock deformations in five outcrops of folds with flat-lying foliation (Sh) at Taimali, Taiwan.
The study region, which is located at the subduction-collision conjunction, southeastern Taiwan, consists of overturned Miocene deposits having undergone lowest-grade metamorphism and ductile-brittle deformation during the Late Cenozoic Penglai Orogeny. There lies a set of flat-lying foliation (Sh) and ESE-trending stretch lineation ( L ). The deformation history was evaluated using incremental strain indicators and microstructures. Observed phenomena are described as follows: (1) the antitaxial overgrowths of fibrous quartz are developed in pressure shadows of pyrite object; (2) non-coaxial strain was indicated by fibers on both cleavage plane (XY) and cleavage-perpendicular plane (XZ); (3) in the XY plane, the radial fibers over the pyrite are prominent and are of the last deformation stage; (4) the rotation directions of pressure shadows in rocks of different limbs were the same on the XY plane, which indicated the pressure shadows have not been affected by folding; (5) the deformation recorded by pressure shadows on the YZ plane in rocks of different limbs of the Jinlun antiform was symmetrical with respect to the fold axial plane. These results show that the deformation history was triclinic deformation and vertical flattening is strong during exhumation in this region. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-13T15:18:17Z (GMT). No. of bitstreams: 1 ntu-97-R95224105-1.pdf: 13519473 bytes, checksum: c72a8b043b7ac72120eac03673c8ddf4 (MD5) Previous issue date: 2008 | en |
| dc.description.tableofcontents | 致謝 III
摘要 V Abstract VII 目錄 IX 圖目錄 XII 表目錄 XV 第一章 緒論 1 1.1研究目的及動機 1 1.2 研究區域之地理位置 8 1.3 研究區域之地質背景與前人研究 9 第二章 研究方法 18 2.1 野外工作 18 2.2 室內工作 23 2.2.1資料處理 23 2.2.2切製定向岩石標本 23 2.2.3 薄片的觀察及描述 26 2.2.4 資料分析 26 第三章 應變分析 — 壓影纖維分析 27 3.1前言 27 3.2 壓影纖維的生成方式與分類 27 3.3 壓影纖維分析 31 3.3.1 壓影纖維構造分析 31 3.3.1 壓影纖維增量應變分析 32 3.4 壓影纖維分析結果 36 3.4.1 壓影纖維構造分析結果 36 3.4.2 壓影纖維增量應變分析結果 41 第四章 應變分析- 磁感率異向性 44 4.1 前言 44 4.2 磁感率異向性分析原理 44 4.3 磁感率異向性資料及分析結果 45 4.3.1 磁感率異向性推得應力方向 46 4.3.2 磁性線理與磁性葉理以及磁感率異向性 49 第五章 地質構造與構造演化史 50 5.1 前言 50 5.2 中視尺度構造之調查 50 5.2.1 壓影纖維構造分析之露頭調查 50 5.2.2 剪切帶及斷層分布情形 53 5.3 構造分期 57 5.3.1 石英脈分期 57 5.3.2 其他構造分期 60 5.3.3 初步的構造演變歷史 62 第六章 討論 64 6.1 次水平葉理面生成之原因 64 6.2 次水平葉理面呈波浪狀分布之原因 69 6.3 快速抬升造成的效應 72 6.4 探討壓影纖維構造在XY面上的空間分佈之原因 76 6.5 探討壓影纖維構造在XZ及YZ面上的空間分佈之原因 80 6.6壓影纖維構造的應用性 82 6.7 磁感率異向性的應用性 83 6.8 巨視運動學 85 6.9 隱沒至碰撞的過度帶之變形作用 89 第七章 結論 90 參考文獻 92 中文部份 92 英文部分 93 附件一 101 圖版一 110 圖版二 120 | |
| dc.language.iso | zh-TW | |
| dc.subject | 太麻里 | zh_TW |
| dc.subject | 壓影纖維構造 | zh_TW |
| dc.subject | 變形歷 | zh_TW |
| dc.subject | 史 | zh_TW |
| dc.subject | 壓扁效應造成的葉 | zh_TW |
| dc.subject | 隱沒-碰撞的過渡帶 | zh_TW |
| dc.subject | flat-lying foliation | en |
| dc.subject | Taimali | en |
| dc.subject | subduction-collision conjunction | en |
| dc.subject | pressure shadows | en |
| dc.subject | strain history | en |
| dc.title | 利用微構造分析太麻里地區的變形歷史 | zh_TW |
| dc.title | Using microstructures to analyze the deformation
history Taimali area, southeastern Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 96-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 張中白 | |
| dc.contributor.oralexamcommittee | 葉恩肇,朱傚祖,詹瑜璋 | |
| dc.subject.keyword | 壓影纖維構造,變形歷,史,壓扁效應造成的葉,理,隱沒-碰撞的過渡帶,太麻里, | zh_TW |
| dc.subject.keyword | pressure shadows,strain history,flat-lying foliation,subduction-collision conjunction,Taimali, | en |
| dc.relation.page | 99 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2008-07-25 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| Appears in Collections: | 地質科學系 | |
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| File | Size | Format | |
|---|---|---|---|
| ntu-97-1.pdf Restricted Access | 13.2 MB | Adobe PDF |
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