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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 鄧屬予 | |
| dc.contributor.author | Chao-Ming Chuang | en |
| dc.contributor.author | 莊釗鳴 | zh_TW |
| dc.date.accessioned | 2021-05-20T21:47:11Z | - |
| dc.date.available | 2010-08-10 | |
| dc.date.available | 2021-05-20T21:47:11Z | - |
| dc.date.copyright | 2010-08-10 | |
| dc.date.issued | 2010 | |
| dc.date.submitted | 2010-08-04 | |
| dc.identifier.citation | 參考文獻
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(1992) Transgressive barrier island and estuarine systems: in Walker, R. G. and James, N. P. ed., Facies Models Response to Sea Level Change, Geological Association of Canada, 157-179. Reading, H. G., and Collinson, J. D. (1996) Clastic coast. In: Reading, H.G. ed., Sedimentary Environments: Processes, Facies and Stratigraphy, 3rd Edition, Blackwell Scienc, Oxford, 154-231. Retalla, G. J. (1997) A color guide to paleosols: John Wiley and Sons, England, pp.175pp. Soons, J. M., Shulmeister, J., and Holt, S. (1997) The Holocene evolution of a well nourished gravelly barrier and lagoon complex, Kaitorete 'Spit', Canterbury, New Zealand: Marine Geology, 138, 69- 90. Tien, J. L., Wang, W. S., Chu, C. J., and Chen, C. H. (1994) The depositional time of the Linkou Formation as revealed by the zircon FTD ages for Quaternary volcanic rocks in northern Taiwan: Journal of the Geological Society of China, 37, 189-214. Tseng, M. H., Liew, P. M., Chi, W. R., and Shih, T. S. (1992) Pollen analysis of the Tananwan formation, Northern Taiwan: Journal of the Geological Society of China, 35, 247-259. Visser, M. J. (1980) Neap- spring cycles reflected in Holocene subtidal large- scale bedform deposits: a preliminary note: Geology, 8, 543-546. Wang, C. M. (1969) Petrology and origin of the Linkou Gravel in Taipei, Taiwan, China: Proceedings of the Geological Society of China, No. 12, 49-64. Wescott, W. A. and Ethridge, F. G. (1980) Fan-delta sedimentology and tectonic setting-Yallahs fan delta, southeast Jamaica: American Association of Petroleum Geologists Bulletin, 64, 374-399. Walker, R. G., and Plint, A. G. (1992) Wave and storm- dominated shallow marine systems. In: Walker, R. G. and James, N. P., ed., Facies Models Response to Sea Level Change, Geological Association of Canada, 219-238. Yagishita, K. (1997) Paleocurrent and fabric analyses of fluvial conglomerates of the Paleogene Noda Group, northeast Japan: Sedimentary Geology, 109, 53-71. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/10654 | - |
| dc.description.abstract | 大南灣層出露在林口台地的西北部，為一砂泥夾薄礫質的地層，與礫石質的林口層為同時異相。大南灣層的沉積環境已有多年的研究，但至今仍無共識。有鑑於此，本研究在大南灣層中，選取七條溪谷剖面進行野外調查，並收集地層及古水流資料進行沉積相分析，以推斷大南灣層的沉積環境。
根據沉積相分析的結果，大南灣層中有顆粒支持礫岩相，代表高濃度洪流及拖曳水流作用；砂岩相中有圓丘狀及低角度槽狀的交錯層理，代表受暴風波浪作用；砂泥互層相中則有含泥紋的波痕，代表受潮汐作用。這些岩相特徵顯示大南灣層為沖積扇三角洲外緣之堆積物，同時受到河流、波浪及潮汐的交互作用。它的岩相可組合為遠端辮狀水道、泛濫平原、決堤水道、潮坪、潟湖/海灣、障壁島/海灘、沼澤及濱面等八種沉積相。 藉由各溪谷剖面的沉積相分佈與變化，可推知早期扇洲之主河道在現今汕頭溪的位置出海；河口以西介於寶斗溪至林口溪之間，則以濱面、障壁島/海灘及潟湖/海灣的沉積環境為主。隨著主河道向西遷移，河道礫石開始與潟湖/海灣及障壁島砂泥層交互出現。期間經歷兩次大規模相對海侵期後，沉積環境轉變為開放性潟湖/海灣。最終隨著扇洲向海側加積，河道堆積物將潟湖/海灣的環境覆蓋。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-05-20T21:47:11Z (GMT). No. of bitstreams: 1 ntu-99-R95224116-1.pdf: 7791501 bytes, checksum: a03bcd0a6121d6214e6ba4c10766422e (MD5) Previous issue date: 2010 | en |
| dc.description.tableofcontents | 目 錄
口試委員會審定書……………………………………………………………………I 誌謝……………………………………………………………………………………II 中文摘要………………………………………………………………………………III 英文摘要………………………………………………………………………………IV 目錄……………………………………………………………………………………V 圖目…………………………………………………………………………………VIII 表目……………………………………………………………………………………X 第一章 前言……………………………………………………………………………1 1-1 地質概況…………………………………………………………………………1 1-2 地層年代…………………………………………………………………………2 1-3 沉積環境…………………………………………………………………………3 1-4 研究動機與目的…………………………………………………………………3 第二章 地層架構………………………………………………………………………5 2-1 前人研究…………………………………………………………………………5 2-2 本研究之地層架構………………………………………………………………5 第三章 研究方法………………………………………………………………………8 3-1 沉積相分析………………………………………………………………………8 3-2 古水流測量………………………………………………………………………8 第四章 岩相…………………………………………………………………………10 4-1 顆粒支持礫岩相Gcm……………………………………………………………10 4-1-1 顆粒支持礫岩相(a) Gcm(a)……………………………………………………10 4-1-2 顆粒支持礫岩相(b) Gcm(b)……………………………………………………12 4-2 透鏡狀礫岩相Glen………………………………………………………………12 4-2-1 透鏡狀礫岩相(a) Glen(a)………………………………………………………12 4-2-2 透鏡狀礫岩相(b) Glen(b)………………………………………………………12 4-3 平板狀交錯層理砂岩相Sp………………………………………………………15 4-3-1 平板狀交錯層理砂岩相(a)……………………………………………………15 4-3-2 平板狀交錯層理砂岩相(b)……………………………………………………15 4-4 槽狀交錯層理砂岩相St…………………………………………………………15 4-5 圓丘狀及低角度槽狀交錯層理砂岩相Sst………………………………………17 4-6 水平與低角度交錯層理砂岩相Slh……………………………………………18 4-7 塊狀砂岩相Sm…………………………………………………………………18 4-8 殘存紋理砂岩相Smb……………………………………………………………18 4-9 波痕砂泥岩互層相SMt…………………………………………………………18 4-10 波狀及透鏡狀層理砂泥互層相SMw…………………………………………21 4-11塊狀泥岩相Mmb………………………………………………………………21 4-12 斑駁狀泥岩相Mmo……………………………………………………………21 4-13 淡紅色泥岩相Mmr…………………………………………………………….21 4-14 平行紋理泥岩相Mh……………………………………………………………23 4-15 旋捲變形泥岩相Mv……………………………………………………………24 第五章 沉積相模式與沉積相組合…………………………………………………25 5-1 沉積相模式………………………………………………………………………25 5-2 近端辮狀水道……………………………………………………………………27 5-3 遠端辮狀水道……………………………………………………………………27 5-4 泛濫平原…………………………………………………………………………28 5-5 決堤水道…………………………………………………………………………28 5-6 潮坪………………………………………………………………………………28 5-7 障壁島/海灘……………………………………………………………………29 5-8 濱面………………………………………………………………………………29 5-9 潟湖/海灣………………………………………………………………………30 5-10 沼澤……………………………………………………………………………30 第六章 大南灣層的沉積環境………………………………………………………36 6-1 垂直沉積序列變化………………………………………………………………36 6-2 側向沉積序列變化………………………………………………………………37 6-3 沉積環境演化……………………………………………………………………37 第七章 結論…………………………………………………………………………41 參考文獻………………………………………………………………………………42 附錄、各溪谷剖面沉積地層柱………………………………………………………48 附錄一、林口溪地層柱………………………………………………………………49 附錄二、嘉寶溪地層柱………………………………………………………………52 附錄三、寶斗溪地層柱………………………………………………………………53 附錄四、瑞樹坑溪地層柱……………………………………………………………56 附錄五、後坑溪、汕頭溪地層柱……………………………………………………58 附錄六、紅水仙溪地層柱……………………………………………………………61 圖 目 圖一、地質背景…………………………………………………………………………1 圖二、研究區域露頭位置圖……………………………………………………………4 圖三、本研究對林口台地之岩石地層架構……………………………………………7 圖四、前人及本研究之地層分類………………………………………………………7 圖五、沉積相分析流程圖………………………………………………………………9 圖六、顆粒支持礫岩相(a)……………………………………………………………13 圖七、顆粒支持礫岩相(b)……………………………………………………………13 圖八、透鏡狀礫岩相(a)………………………………………………………………14 圖九、透鏡狀礫岩相(b)………………………………………………………………14 圖十、平板狀交錯層理砂岩相(a)……………………………………………………16 圖十一、平板狀交錯層理砂岩相(b)…………………………………………………16 圖十二、槽狀交錯層理砂岩相 ………………………………………………………17 圖十三、圓丘狀及低角度槽狀交錯層理砂岩相 ……………………………………17 圖十四、水平與低角度交錯層理砂岩相 ……………………………………………19 圖十五、塊狀砂岩相 …………………………………………………………………19 圖十六、殘存紋理砂岩相 ……………………………………………………………20 圖十七、波痕砂泥互層相……………………………………………………………20 圖十八、波狀及透鏡狀砂泥互層相…………………………………………………22 圖十九、塊狀泥岩相 …………………………………………………………………22 圖二十、斑駁狀泥岩相………………………………………………………………23 圖二十一、淡紅色泥岩相……………………………………………………………23 圖二十二、平行紋理泥岩相…………………………………………………………24 圖二十三、旋捲變形泥岩相…………………………………………………………24 圖二十四、大南灣層的沉積相模式…………………………………………………25 圖二十五、近端辮狀水道沉積相組合………………………………………………31 圖二十六、遠端辮狀水道沉積相組合………………………………………………31 圖二十七、泛濫平原沉積相組合……………………………………………………32 圖二十八、決堤水道沉積相組合……………………………………………………32 圖二十九、潮坪沉積相組合…………………………………………………………33 圖三十、礫石質障壁島/海灘沉積相組合……………………………………………33 圖三十一、濱面、砂質障壁島/海灘沉積相組合……………………………………34 圖三十二、潟湖/海灣沉積相組合……………………………………………………34 圖三十三、沼澤沉積相組合…………………………………………………………35 圖三十四、各溪谷剖面沉積環境柱狀圖……………………………………………39 圖三十五、沉積環境演化圖…………………………………………………………40 表 目 表一、林口台地地層之年代研究………………………………………………………2 表二、岩相分類………………………………………………………………………11 表三、沉積相組合……………………………………………………………………26 | |
| dc.language.iso | zh-TW | |
| dc.title | 林口台地大南灣層的沉積環境 | zh_TW |
| dc.title | Depositional environment of Tanawan Formation, Linkou Tableland | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 98-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳文山,劉平妹,袁彼得,吳樂群 | |
| dc.subject.keyword | 大南灣層,林口層,沉積相,沖積扇三角洲, | zh_TW |
| dc.subject.keyword | Tananwan Formation,Linkou Formation,Depositional facies,Fan delta, | en |
| dc.relation.page | 62 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2010-08-05 | |
| 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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