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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 俞何興 | |
| dc.contributor.author | Yi- Huei Chang | en |
| dc.contributor.author | 張亦慧 | zh_TW |
| dc.date.accessioned | 2021-06-15T01:19:59Z | - |
| dc.date.available | 2009-07-29 | |
| dc.date.copyright | 2009-07-29 | |
| dc.date.issued | 2009 | |
| dc.date.submitted | 2009-07-26 | |
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Intraslope basin, seismic facies and sedimentary processes in the Kaoping slope, offshore southwestern Taiwan. Terr. Atmos. Ocean. Sci. 17, 659-677. Yu, H. S., Chiang, C. S., Shen, S. M., 2009. Tectonically active sediment dispersal system in SW Taiwan margin with emphasis on the Gaoping (Kaoping) submarine canyon. J. Mar. Sys. 76, 369-382. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/42694 | - |
| dc.description.abstract | 利用多頻道震測剖面及水深資料，討論台灣西南海域枋寮海底峽谷之沉積/形貌特徵與沉積物散佈交互關係。
依照峽谷流徑可將枋寮海底峽谷分成上段及下段峽谷，另外峽谷末端有一沉積物堆積區。上段峽谷頭部發展於棚緣處並嵌入陸棚，是一陸棚嵌入(shelf-indenting)峽谷，從峽谷頭部沿等深線往下部陸坡延伸，終止在600 公尺水深處，長約10 公里，谷軸為南北向，橫剖面呈V 型形貌，震測剖面顯示有崩移及側壁截切現象，說明峽谷受到侵蝕作用，沉積物可能形成濁流侵蝕峽谷或僅通過(bypass)峽谷；下 段峽谷從600 公尺發展至900 公尺水深處，長約30 公里，谷軸轉為西南向，橫剖面呈U 型形貌，震測剖面顯示有崩移及側壁有截切現象，峽谷寬度增加，谷底有沉積物充填，說明峽谷受側向侵蝕作用，谷軸及谷底受沉積作用，下段峽谷同時受侵蝕及沉積作用交互影響；峽谷末端約900~1000 公尺水深處，峽谷特徵不明顯，地形起伏小，有沉積物充填舊水道大部分的空間，可視為沉積物傳輸通道的終點 或是沉積物溢出的沉積中心，主要受沉積作用影響堆積成約400 平方公里的海底扇，並推論為發展初期的小型海底扇。 枋寮峽谷的頭部形狀為短直線型，僅稍微嵌入棚緣處，與其他大型陸棚嵌入峽谷枋寮峽谷嵌入陸棚程度較小。陸棚嵌入峽谷頭部主要有圓形劇場型(amphitheatre-shape)及狹窄的直線型兩種形狀，但依水深圖無法將枋寮峽谷頭部做適當的分類。推論台灣島未來若產生抬昇等地體運動，會因侵蝕基準面下降在棚緣附近產生連續性的小型峽谷，並且整體往頭部侵蝕的情形會增強，則枋寮峽谷的頭部會趨向圓形劇場型。枋寮峽谷末端嘴部區域無水道限制沉積物傳輸且坡度減緩，則沉積物失去動力容易堆積成海底扇，但上游提供有限的沉積物量，使枋寮峽谷發展至上部陸坡即產生堆積，推論沉積物量不增加的情形下，不易繼續發展成大型海底扇。 枋寮海底峽谷的沉積物散佈(sediments dispersal)與相似地質條件的高屏峽谷沉積物來源(source)及匯集處(sink)不同。枋寮海底峽谷的頭部附近無大型河流提供沉積物注入峽谷，有限的沉積物量影響峽谷發展，沉積物源僅依賴峽谷頭部附近沉積物不穩定崩移的物質；而高屏海底峽谷的頭部和高屏溪連接，提供陸源沉積物直接注入峽谷頭部，有足夠的沉積物源可以影響峽谷發展；枋寮峽谷的沉積物匯集於上部陸坡的小型海底扇，而高屏峽谷的匯集處是深海的馬尼拉海溝。雖兩者來源與匯集處不同，但皆為輸送陸棚沉積物的通道。所以枋寮峽谷可被視為一個沉積物來源有限、低容量，僅輸送淺海沉積物至上部陸坡的通道。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-15T01:19:59Z (GMT). No. of bitstreams: 1 ntu-98-R96241301-1.pdf: 5029068 bytes, checksum: bfc043bebb1b5889f4267e990cf10e69 (MD5) Previous issue date: 2009 | en |
| dc.description.tableofcontents | 目錄
摘要...........................................i 目錄..........................................iii 圖目錄........................................iv 第一章 序論....................................1 第二章 研究背景 2.1 區域地質...................................7 2.1.1 台灣西南海域地體構造.....................7 2.1.2 台灣西南海域地形特徵.....................8 2.2 前人研究...................................12 2.3 研究目的...................................16 第三章 研究資料與方法 3.1 研究方法...................................17 3.2 水深資料...................................17 3.3 反射震測資料.............................,.18 第四章 討論 4.1 枋寮峽谷的地形與形貌.......................20 4.1.1 枋寮峽谷的頭部...........................26 4.1.2 枋寮峽谷的末端...........................28 4.1.3 枋寮峽谷可能的演化模式...................33 4.2 枋寮峽谷的沉積物散佈.......................35 第五章 結論與未來展望 5.1 結論.......................................42 5.2 未來展望...................................43 參考文獻.......................................44 | |
| dc.language.iso | zh-TW | |
| dc.subject | 沉積物散佈 | zh_TW |
| dc.subject | 台灣 | zh_TW |
| dc.subject | 海底峽谷 | zh_TW |
| dc.subject | 震測 | zh_TW |
| dc.subject | 地形 | zh_TW |
| dc.subject | submarine canyon | en |
| dc.subject | Taiwan | en |
| dc.subject | seismic | en |
| dc.subject | sediment dispersal | en |
| dc.subject | morphology | en |
| dc.title | 台灣西南海域枋寮海底峽谷的沉積/形貌特徵與沉積物散佈 | zh_TW |
| dc.title | Morpho/sedimentary features and sediment dispersal of the Fangliao Submarine Canyon offshore SW Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 97-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳汝勤,洪奕星,張翠玉 | |
| dc.subject.keyword | 海底峽谷,地形,沉積物散佈,震測,台灣, | zh_TW |
| dc.subject.keyword | submarine canyon,morphology,sediment dispersal,seismic,Taiwan, | en |
| dc.relation.page | 50 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2009-07-27 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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