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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 鄧屬予(Louis Suh-Yui Teng) | |
| dc.contributor.author | Meng-Lun Li | en |
| dc.contributor.author | 李孟綸 | zh_TW |
| dc.date.accessioned | 2021-06-17T03:15:16Z | - |
| dc.date.available | 2018-07-19 | |
| dc.date.copyright | 2018-07-19 | |
| dc.date.issued | 2018 | |
| dc.date.submitted | 2018-07-09 | |
| dc.identifier.citation | Allmendinger, R. W., Cardozo, N., & Fisher, D. M. (2011). Structural geology algorithms: Vectors and tensors: Cambridge University Press.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/69421 | - |
| dc.description.abstract | 雪山山脈東側與宜蘭平原交界的丘陵地區，在地形上為一明顯的構造線形。前人推斷此地形特徵為活斷層所致，但並未提出明確的地質證據。本研究利用數值地形分析配合影像判釋和野外調查，以探討該丘陵區的裂縫系統及構造特徵。
為求得地形上之裂縫特性，本研究透過日照陰影圖及曲率地圖強化線形特徵，以勾繪該丘陵區的斷層跡線，並利用構造等高線法求得斷層之位態後，再比對曲率地圖以區分斷層滑移屬性。大體而言，本區充斥著短小的斜滑斷層，位態為東北-西南與西北-東南兩走向，其分別向東南傾斜40至50度及向東北或西南傾斜約70度，兩相夾70至90度角。 地形上之斷層跡線亦可在野外確實追蹤，其斷層毀壞帶及核心皆可明確查驗，其核心伴隨有密集的破裂面、斷層角礫岩、斷層泥及斷層擦面。實地量測斷層擦面之位態後，本研究發現其與地形判釋之結果大致相同，其中，有東北-西南向之左斜滑斷層，傾角多陡立，上有向東北傾10至20度的擦線。而西北-東南向的右斜滑斷層，斷層面呈陡立或略向東北傾，擦線向東南傾沒10度。 綜合地形判釋及野外調查結果，可知宜蘭平原西側丘陵地區為一斜滑斷層為主的破碎帶，統整這些裂縫與它們的滑動方向後，可知其反應西北-東南向拉張，與衛星定位系統(GPS)所展現之方向一致，可顯示地形之特徵與後造山期的斜張作用有關。 | zh_TW |
| dc.description.abstract | The northwestern edge of Yilan Plain is marked by a topographic lineament cutting through to the Hsuehshan Range. Previous researchers usually regarded the northwestern edge of Yilan Plain as an active normal fault according to its topography features and associated surface deformation but presented no structural evidence. With combination of Digital Terrain Model analysis, lineament interpretation and field survey, we examine the fracture systems in the area along the eastern edge of the Hsuehshan Range to explore the structural characteristics of the fractures zone.
We first enhanced lineament features from hillshade and curvature thematic maps to extract faulting traces on the eastern Hsuehshan Range. Then, we used structural contours method, in association with the curvature map, to obtain the fault attitude and attribute. The result show that the major fractures are NE-SW oblique-slip faults with dipping angle 55~80゜to the SE and NW-trending vertical oblique-slip faults. The fault traces found in the field and generally associated with fault breccias, gouges and slickensides. One NE-trending sinistral oblique-slip faults are marked with vertical dipping and slickenlines about 20゜plunging to the NE; whereas another two vertical, NW-striking dextral oblique-slip faults with slickenlines about 10゜plunging to the SE. In sum, the fractures zone is composed of oblique-slip fractures striking NE-SW and NW-SE. The movements of those fractures, possibly caused by post-collision oblique extension in northeastern Taiwan, are in accordance with the strain patterns deduced from Global Position System records in the study area. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-17T03:15:16Z (GMT). No. of bitstreams: 1 ntu-107-R04224103-1.pdf: 15968109 bytes, checksum: e1c2bacdc500cf1fb50eb3e1aad277b9 (MD5) Previous issue date: 2018 | en |
| dc.description.tableofcontents | 口試委員會審定書 I
謝誌 II 中文摘要 III ABSTRACT IV 目錄 V 圖目錄 VI 第一章. 緒論 1 1.1引言 1 1.2 地質背景 3 1.3前人研究 5 1.4研究動機及目的 9 第二章. 研究方法 10 2.1數值地形分析 11 2.1.1基本原理 11 2.1.2資料運算 13 2.1.3線形判釋 14 2.1.4曲率分析 16 2.1.5斷層屬性分類 20 2.1.6裂縫位態及構造等高線 24 2.2野外實查 26 2.2.1野外調查區域 26 2.2.2分辨斷層屬性 27 第三章. 野外裂縫實查 30 3.1金面山地區 30 3.2粗坑及破礑溪地區 35 第四章. 裂縫分佈與屬性 39 4.1裂縫屬性及位態 39 4.2北段及南段破碎帶分佈 42 第五章. 討論與結論 46 5.1 地形特徵與裂縫 46 5.2金面山地區構造地質彙整 46 5.3破碎帶分佈及屬性 48 5.4破碎帶應力狀態 49 5.5 結論 52 參考文獻 53 附錄:北段破碎帶位態資料 57 附錄:南段破碎帶位態資料 60 | |
| dc.language.iso | zh-TW | |
| dc.subject | 活斷層 | zh_TW |
| dc.subject | 大地應變 | zh_TW |
| dc.subject | 斜滑斷層 | zh_TW |
| dc.subject | 線形判釋 | zh_TW |
| dc.subject | ground strain | en |
| dc.subject | interpretation of lineaments | en |
| dc.subject | oblique-slip faults | en |
| dc.subject | active fault | en |
| dc.title | 宜蘭平原西側雪山山脈之構造地形分析初探 | zh_TW |
| dc.title | Primary Study of Morphotectonic Analysis in the Hsuehshan Range of western Yilan Plain, Northeastern Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 106-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 李錫堤,葉恩肇,陳柔妃,王昱 | |
| dc.subject.keyword | 線形判釋,斜滑斷層,大地應變,活斷層, | zh_TW |
| dc.subject.keyword | interpretation of lineaments,oblique-slip faults,ground strain,active fault, | en |
| dc.relation.page | 62 | |
| dc.identifier.doi | 10.6342/NTU201801289 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2018-07-09 | |
| 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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