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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 劉家瑄(Char-Shine Liu) | |
dc.contributor.author | Tzu-Ting Chen | en |
dc.contributor.author | 陳姿婷 | zh_TW |
dc.date.accessioned | 2021-06-17T01:09:23Z | - |
dc.date.available | 2021-02-06 | |
dc.date.copyright | 2020-02-06 | |
dc.date.issued | 2020 | |
dc.date.submitted | 2020-01-19 | |
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dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/66843 | - |
dc.description.abstract | 臺灣西南海域的增積岩體受到擠壓的應力,產生許多褶皺與逆衝斷層,也提供了流體移棲的管道。本研究利用水下無人載具(autonomous underwater vehicle,簡稱AUV)所收集的高解析水深資料與回散射(backscatter)影像,來了解於西南海域三個增積海脊上受流體活動所造成的海床特徵分布。兩種特殊海床形貌分別為位在海脊兩側斜坡的彗星狀孔洞(comet-shaped depressions,簡稱CSD)與多分布於海脊軸部的海底隆堆(pingo)。由淺至深的地層剖面協助本研究評估增積岩體中構造對於流體移棲與其海床形貌的影響,其剖面顯示海床下具有許多切過海底仿擬反射訊號(BSR)至淺部的傾斜高振幅反射層面(high amplitude reflector packages)與煙囪(seismic chimneys)、裂隙等震測特徵,推測(1)流體能沿著這些傾斜層面向淺部移棲、(2)隆堆下方具有大量的流體填充。本研究同時藉由水下遙控載具(remotely-operated vehicle,簡稱ROV)以及拖曳式海床觀測系統(Ocean Floor Observation System,簡稱OFOS)所收集的海底影像、岩石標本、管蟲以及壓式短岩心(push core),搭配AUV高解析地形來進一步分析流體滲漏的形貌演化與差異,其結果顯示(3)隆堆上岩石標本的低δ13C值(−39.9 and −44.3 per mil VPDB),為受到甲烷氣移棲而產生的自生性碳酸鹽礁、(4)具有淺硫酸鹽-甲烷界面(4公分)的黑白色菌叢位於冷泉系統兩側,可望作為海床滲漏的特徵、(5)冷泉系統兩側具有旺盛的冒氣特徵與生物富集並隨地形而有所差異,可能為流體向外側遷移的證據。另一方面,在搭配本研究建立的海床底質分類法後,我們分析了具流體滲漏特徵的海床沉積物環境與其形貌差異,並建議(6)這些孔洞的尺寸受裂隙與出露層面的分布較沉積環境影響大。最後,CSD與隆堆的形貌與形成機制也指示(7)這兩種受流體活動所造成的海床特徵有著不同的滲流速率,海底隆堆是隨時間緩慢而連續地發展,但彗星形孔洞可能是受到地震事件觸發所形成。因此,彗星狀孔洞有可能指示著在短時間釋出大量氣體的事件,值得後續投入更多的研究。 | zh_TW |
dc.description.abstract | Folds and thrust faults developed in accretionary wedge off southwestern Taiwan may provide conduits for fluid migration from deep strata to seafloor as there are many seafloor seepage features formed in this area. High-resolution bathymetric data and backscatter images collected using an autonomous underwater vehicle (AUV) over three accretionary ridges are analyzed to better understand the characters, distribution and development of the observed seepage features. Two types of seepage features are revealed: comet-shaped depressions (CSD) occur on flanks of the ridges studied, and pingos mostly occur on or near the apexes of these ridges. In addition, these features overlie areas where multichannel seismic reflection profiles show bottom simulating reflectors (BSR) together with seismic chimneys and high amplitude reflector packages along some dipping strata extending from below BSR to near seafloor. We suggest that (1) these CSD are related to gas seepages as the fluid possibly migrates along the dipping strata and then blowouts on the seafloor where the dipping strata were cut at seafloor, forming these depressions; and (2) there is a large volume of fluid accumulated under the pingos. In addition, seafloor images, rock samples, tubeworms, and push cores have also been collected by ocean floor observation system (OFOS) and remotely-operated vehicle (ROV) to evaluate the evolution of seepages. Our results show that (3) the rock samples have low δ13C values, indicating the source of methane-rich fluid; (4) the microbial mat on the side of a cold seep could be an indicator of seepage feature because the depth of the sulfate-methane interface from the push cores taken at the microbial mat site is less than four centimeters; (5) strong flares with enriched biological communities are on both sides of the cold seep system, providing the evidence of lateral fluid migration. Based on analyzing the sub-bottom profiles using the automatic seabed classification method, we also suggest that (6) structures have more influence on the seepage characteristics than types of seafloor sediments. Finally, we surmise that (7) two types of seepage features were formed at different seep rates, with pingos developed slowly and continuously over time, while CSD formed in discrete events, perhaps triggered by large earthquakes. Our results suggest more studies should be carried out for these seepage features. | en |
dc.description.provenance | Made available in DSpace on 2021-06-17T01:09:23Z (GMT). No. of bitstreams: 1 ntu-109-D03241004-1.pdf: 53686737 bytes, checksum: bc45c910749e40cb6684a4001b547452 (MD5) Previous issue date: 2020 | en |
dc.description.tableofcontents | 中文摘要 i
Abstract ii 圖 目 錄 v 表 目 錄 vii 第1章 緒論 1 1.1 前言 1 1.2 臺灣西南海域的海床流體滲漏特徵與相關研究 2 1.3 區域沉積環境與沉積物特性分析 3 1.4 研究動機 4 1.5 論文架構 5 第2章 文獻探討 10 2.1 區域地質特徵 10 2.2 海床流體滲漏特徵之研究 13 2.3 近海床觀測的研究貢獻及現況 17 第3章 研究資料與方法 32 3.1 資料來源 32 3.2 水深資料處理流程 34 3.3 海床特性與地層剖面處理流程 35 3.4 底質影像分類法 36 3.5 碳14定年與碳氧同位素分析 37 第4章 海床形貌特徵與沉積分析 48 4.1 區域地形特徵 48 4.2 細微海床特徵 48 4.3 地層構造特徵 50 4.4 海床沉積特徵 51 4.5 岩石樣本碳14定年與碳氧同位素分析 51 第5章 討論 72 5.1 比對過往海床流體滲漏特徵形貌的分布 72 5.2 比較不同麻坑形貌 72 5.3 海床流體滲漏特徵形貌的形成 73 5.4 冷泉系統的生長方向 74 5.5 海床底質與構造對彗星狀孔洞的影響 75 5.6 增積岩體上海床流體滲漏特徵的演化 76 5.7 海床彗星狀孔洞的觸發事件 77 5.8 海床流體滲漏特徵的形貌演化差異 78 第6章 結論 87 參考文獻 89 附錄一 底質分類法簡述 99 | |
dc.language.iso | zh-TW | |
dc.title | 臺灣西南海域增積海脊受流體活動所造成之海床特徵 | zh_TW |
dc.title | Seafloor Features Induced by Fluid Activities on Accretionary Ridges off Southwestern Taiwan | en |
dc.type | Thesis | |
dc.date.schoolyear | 108-1 | |
dc.description.degree | 博士 | |
dc.contributor.coadvisor | 蘇志杰(Chih-Chieh Su) | |
dc.contributor.oralexamcommittee | 王詠絢(Yun-Shuen Wang),許樹坤(Shu-Kun Hsu),戚務正(Wu-Cheng Chi),陳松春(Song-Chuen Chen),景國恩(Kuo-En Ching) | |
dc.subject.keyword | 水深,天然氣水合物,流體移棲,自生性碳酸鹽礁,水下載具,底質分類, | zh_TW |
dc.subject.keyword | Bathymetry,Gas hydrate,Fluid migration,Authigenic carbonate,Underwater vehicle,Seabed classification, | en |
dc.relation.page | 102 | |
dc.identifier.doi | 10.6342/NTU202000192 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2020-01-20 | |
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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