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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳文山(Wen-Shan Chen) | |
| dc.contributor.author | Fei-Hong Zhou | en |
| dc.contributor.author | 周飛宏 | zh_TW |
| dc.date.accessioned | 2021-06-13T02:29:44Z | - |
| dc.date.issued | 2007 | |
| dc.date.submitted | 2007-01-25 | |
| dc.identifier.citation | 中文部分：
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A. and van Wagoner, J. eds. Sea-Level Change: an Integrated Approach, SEPM, Spec. Pub, 42, 39-46. Van Wagoner, J.C., Mitchum, R.M.Jr., Campion, K.M. and Rahmanian, V.D. (1990) Siliciclastic Sequence Stratigraphy in Well Logs, Cores, and Outcrops：Concepts for High-resolution Correlation of Time and Facies: Am. Assoc. Petro. Geol. Methods in Exploration Ser., 7, 55pp. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/31099 | - |
| dc.description.abstract | 為了了解台南地區的地下構造幾合型態及活動特性，重新進行了岩心紀錄及槽溝工作。由地層層序與古環境分析，估算此區地殼變動速率。研究結果顯示，台南台地的隆起受地下的台南斷層作用所造成，台南斷層為一朝東傾斜的逆衝斷層，斷層目前處於「鎖定」的狀態且斷層尖端未截切至地表淺層沉積層，但在長期變動下可能已經造成六雙層基盤的錯移。晚更新世以來，在台南斷層的作用下造成台南背斜，伴隨台南背斜的活動造成台南台地變動速率的變化，亦造成台南台地的全新世沉積層產生背斜的構造，台南台地背斜軸部的抬升速率為4.6 mm/yr，並向東與向西兩側遞減至0.6 mm/yr與0.2 mm/yr。後甲里斷層為一向西傾斜的盲斷層，只造成地表全新世沉積層產生褶皺，並在軸部產生數十公分的錯移。中洲台地的隆起因中洲斷層的活動所造成，中洲斷層亦為一向東傾斜的逆衝斷層，斷層目前處於「鎖定」的狀態。在長期變動下，應該已經造成六雙層基盤的錯移，且可能造成全新世沉積層的錯移。晚更新世以來，中洲斷層的作用造成中洲背斜，伴隨中洲背斜的活動使得中洲台地變動速率有不同的變化，亦造成中洲台地的全新世沉積層產生背斜的構造，中洲台地的抬升速率由1.2 mm/yr往東遞增至6.7 mm/yr。 | zh_TW |
| dc.description.abstract | In order to understanding Construct several shutting type attitudes and activity characteristics for the underground of the area of Tainan, have carried on noting down and trough ditch work of drill core again. One layer of preface and ancient environmental analysis, estimate the speed of the crust change of this district by the stratum. The result of study shows, the dislocated upwarping of the Tainan tableland is caused by underground Tainan fault function, Tainan fault that the east slope against thrust fault for one dynasty, state that fault in at present and fault peak the deposit layer to the earth's surface shallow layer to cut , but may already cause the moving by mistake of basement under changing for a long time. Since late Pleistocene, causing the Tainan anticline under the function of Tainan fault, it causes the change of the speed of Tainan tableland change follow Tainan anticlinal activity, it produces anticlinal structure that the ones that also cause the Tainan tableland brand-new to deposit on storey generation, the speed of lifting of the Tainan tableland anticlinal axle department as 4.6 mm/yr, and decrease progressively with both sides westwards to 0.6 mm/yr and 0.2 mm/yr eastwards. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-13T02:29:44Z (GMT). No. of bitstreams: 1 ntu-96-R93224110-1.pdf: 7679661 bytes, checksum: a5651d6c1f71672c9d6ad174ae275c63 (MD5) Previous issue date: 2007 | en |
| dc.description.tableofcontents | 目 錄
頁次 口試委員會審定書------------------------------------------------------------------------------ I 致謝 -------------------------------------------------------------------------------------------------II 摘要 -----------------------------------------------------------------------------------------------IV 目錄 -----------------------------------------------------------------------------------------------VI 表目 ---------------------------------------------------------------------------------------------VIII 圖目 --------------------------------------------------------------------------------------------VIIII 第一章 緒論----------------------------------------------------------------------- 1 1.1 前言-------------------------------------------------------------- 1 1.2 地質背景----------------------------------------------------------------- 2 1.3 研究材料與方法-------------------------------------------------------10 第二章 淺層鑽探的岩心紀錄--------------------------------------------------11 2.1 岩心資料----------------------------------------------------------------11 2.2 岩心地層分佈----------------------------------------------------------14 2.3 沉積相-------------------------------------------------------------------17 2.4 沉積環境體系域-------------------------------------------------------23 2.5 鑽井岩心沉積環境分析----------------------------------------------26 第三章 沉積層序分析-----------------------------------------------------------33 3.1 層序界限與體系域----------------------------------------------------33 3.2 台南地區晚更新世－全新世的層序地層------------------------- 35 3.3 層序對比---------------------------------------------------------------- 42 3.4 末次冰期以來台南地區沉積環境的演化-------------------------47 第四章 後甲里槽溝工作--------------------------------------------------------49 4.1 前人工作----------------------------------------------------------------49 4.2 槽溝位置與地形-------------------------------------------------------50 4.3 槽溝剖面地層----------------------------------------------------------52 4.4 槽溝構造----------------------------------------------------------------55 4.5 岩心剖面地層----------------------------------------------------------55 4.6 構造特性----------------------------------------------------------------56 第五章 地殼變動速率-----------------------------------------------------------61 5.1 地殼變動速率估算法-------------------------------------------------61 5.2 末次冰期以來海水面變動-------------------------------------------62 5.3 台南地區構造變動速率----------------------------------------------63 第六章 討論-----------------------------------------------------------------------73 6.1 台南地區沉積層特性-------------------------------------------------73 6.2 地殼變動速率----------------------------------------------------------75 6.3 台南地區地下構造特性----------------------------------------------78 第七章 結論-----------------------------------------------------------------------85 參考文獻 ----------------------------------------------------------------------------88 附錄 ----------------------------------------------------------------------------------95 | |
| dc.language.iso | zh-TW | |
| dc.subject | 中洲台地 | zh_TW |
| dc.subject | 後甲里斷層 | zh_TW |
| dc.subject | 中洲斷層 | zh_TW |
| dc.subject | 台南斷層 | zh_TW |
| dc.subject | 台南台地 | zh_TW |
| dc.subject | Tainan tableland | en |
| dc.subject | Tainan fault | en |
| dc.subject | Holocene | en |
| dc.title | 從全新世沉積層序探討台南地區褶皺－逆衝斷層帶的構造特性 | zh_TW |
| dc.title | Active structure of fold-and-thrust belt deduced by sequence stratigraphy analysis during the Holocene, Tainan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 95-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 林?文(Qi-Wen Lin),吳樂群(Le-Qun Wu),游能悌(Neng-Ti You) | |
| dc.subject.keyword | 台南台地,中洲台地,台南斷層,中洲斷層,後甲里斷層, | zh_TW |
| dc.subject.keyword | Tainan tableland,Tainan fault,Holocene, | en |
| dc.relation.page | 115 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2007-01-26 | |
| 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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