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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 陳文山 | |
dc.contributor.author | Chih-Hao Chen | en |
dc.contributor.author | 陳志壕 | zh_TW |
dc.date.accessioned | 2021-05-20T20:02:26Z | - |
dc.date.available | 2009-08-20 | |
dc.date.available | 2021-05-20T20:02:26Z | - |
dc.date.copyright | 2009-08-20 | |
dc.date.issued | 2009 | |
dc.date.submitted | 2009-08-19 | |
dc.identifier.citation | 中文部份:
陳文山、楊志成、楊小青、吳樂群、林啟文、張徽正、石瑞銓、林偉雄、李元希、石同生、盧詩丁(2004) 從構造地形探討嘉南地區的活動構造。經濟部中央地質調查所彙刊,第17期,53-77頁。 中國石油公司臺灣油礦探勘總處(1992) 高雄地質圖,比例尺十萬分之一。中國石油公司。 耿文溥(1981) 台南以東丘陵區之地質。經濟部中央地質調查所彙刊,第一號,1-33頁。 周飛宏(2007) 從全新世沉積層序探討台南地區褶皺-逆衝斷層帶的特性。國立台灣大學地質科學研究所碩士論文,共115頁。 陳文山、松多信尚、石瑞銓、楊志成、游能悌、朱耀國、陳志壕、林啟文、劉桓吉、盧詩丁、劉彥求、林燕慧、陳柏村(2009) 臺灣西部平原區隱伏在全新世沉積層下的新期構造-以小崗山斷層為例。經濟部中央地質調查所特刊,第23號 饒瑞鈞、李元希、胡植慶(2008) 地震地質與地變動潛勢分析-地變動監測分析(2/4)。經濟部中央地質調查所97年研究報告,共118頁。 陳于高(1993) 晚更新世以來南台灣地區海水面變化與新構造運動研究。國立台灣大學地質研究所博士論文,共158頁。 景國恩、饒瑞鈞、李建成、胡植慶、侯進雄(2008) 由1995-2005年之GPS觀測資料探討台灣西南部之地殼變形。經濟部中央地質調查所特刊,第20號,17-31頁。 英文部分: Bourgeois, J. (1980) A transgressive shelf sequence exhibiting hummocky stratification: the Cape Sebastian Sandstone (Upper Cretaceous), southwestern Oregon, J. Sedi. Petrol., 50, 681-702. Bown, T. M. and Kraus, M. J. (1987) Integration of channel and floodplain suites, I. Developmental sequence and lateral relations of alluvial paleosols, J. Sedi. Petrol., 57, 587-601. Bull, W. B. 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D. (1978) Lithofacies types and vertical profile models in braided river deposits. In Miall, A. D. (ed) Fluvial Sedimentology. Can. Soc. Petro. Geol. Mem., 5, 579-604. Miall, A. D. (1985) Architectural-element analysis: a new method of facies analysis applied to fluvial deposits. Earth Sci. Rev., 22, 261-308. Miall, A. D. (1992) Alluvial deposits. In Walker, R. G. and James, N. P. (eds) Facies Models: Response to Sea Level Change. Geol. Assoc. Can., Waterloo, Ontario, 119-142. Miall, A. D. (1996) The Geology of Fluvial Deposits-Sedimentary Facies, Basin Analysis, and Petroleum Geology. Springer-Verlag, Berlin, 582pp. Middleton, G. V. and Hampton, M. A. (1973) Sediment gravity flows: mechanics of flow and deposition. In Middleton, G. V. and Bouma, A. H. (eds) Turbidites and Deep-water Sedimentation. Soc. Econ. Paleontol. Mineral. Short Course Notes, Pacific Section, 1-38. Nemec, W. and Steel, R. J. (1984) Alluvial and coastal conglomerates: their significant features and some comments on gravelly mass-flow deposits. In Koster, E. H. and Steel, R. J. (eds) Sedimentology of Gravels and Conglomerates. Can. Soc. Petro. Geol. Mem., 10, 1-31. Pan, Y. S. (1968) Interpretation and seismic coordination of the Bouguer gravity anomalies over southwestern Taiwan: Petrol. Geol. Taiwan, 6, 197-207. Posamentier, H. W. and Vail, P. R. (1988) Eustatic controls on clastic deposition II-sequence and systems tract models. In Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H. W., Ross, C. A. and Van Wagoner, J. (eds) Sea-Level Change: an Integrated Approach. Soc. Econ. Paleontol. Mineral. Spec. Pub., 42, 125-154. Posamentier, H. W., Jervey, M. T. and Vail, P. R. (1988) Eustaic controls on clastic deposition. I - conceptual framework. In Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H. W., Ross, C. A. and Van Wagoner, J. 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(1968) Classification and origin of flaser and lenticular bedding. Sedimentology, 11, 99-104. Rohling, E. J., Fenton, M., Jorissen, F. J., Bertrand, P., Ganssen, G. and Caulet, J.P. (1998) Magnitudes of sea-level lowstands of the past 500000 years. Nature, 394, 162-165. Rust, B. R. (1978) Depositional model for braided alluvium. In Miall, A. D. (ed) Fluvial Sedimentology, Can. Soc. Petro. Geol. Mem., 5, 605-626. Rust, B. R. and Koster, E. H. (1984) Coarse alluvial deposits. In Walker, R. G. (ed) Facies Models, 2nd Edition. Geol. Assoc. Can., Reprint Ser. 1, Waterloo, Ontario, 53-70. Sun, S. C., (1963) The reef limestones and the geologic structures in the vicinity of Kaohsiung city, Taiwan: Mr. Lin’s Jublee Volume, Petrol. Geol. Taiwan, 2, 47-64. Sun, S. C., (1964) Photogeologic study of the Tainan-Kaohsiung coastal plain area, Taiwan: Petrol. Geol. Taiwan, 3, 39-51. Swift, D. J. P., Figueiredo, A. G. Jr., Freeland, G. L. and Oertel, G. F. (1983) Hummocky cross-strstification and megaripples: A geological double standard? J. Sedi. Petrol., 53, 1295-1317. Swift, D. J. P., Philips, S. and Thorne, J. A. (1991) Sedimentation on continental margins, IV: lithofacies and depositional systems. In Swift, D. J. P., Tillman, R. W. and Thorne, J. A. (eds) Shelf Sand and Sandstone Bodies. Spec. Pub. Int. Assoc. Sedi., 14, 89-152. Teng, L. S. (1987) Stratigraphic records of the late Cenozoic Penglai orogeny of Taiwan: Acta Geol. Taiwanica, 25, 205-224. Terwindt, J. H. J. (1988) Palaeo-tidal reconstructions of inshore tidal depositional environments. In de Boer, P. L., van Gelder, A. and Nio, S. D. (eds) Tide-influenced Sedimentary Environments and Facies. Reidel, Dordrecht, 233-263. Vail, P. R. (1987) Seismic stratigraphy interpretation procedure. In Bally, A. W. (ed) Atlas of seismic stratigraphy. Am. Assoc. Petroleum Geology Studies in Geology, 27, 1-10. Van Straaten, L. M. J. U. (1954) Composition and structure of recent marine sediments in the Netherlands Leidse. Geol. Med. XIX, 1-110. Van Straaten, L. M. J. U. (1961) Sedimentation in tidal flat areas. J. Alberta soc. Petrol Geol., 9, 203-226. Van Wagoner, J. C., Posamentier, H. W., Mitchum, R. M., Vail, P. R., Sarg, J. F., Loutit, T. S. and Hardenbol, J. (1988) An overview of the fundamentals of sequence stratigraphy and key definitions. In Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H. W., Ross, C. A. and Van Wagoner, J. (eds) Sea-Level Change: an Integrated Approach. Soc. Econ. Paleontol. Mineral. Spec. Pub., 42, 39-45. 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. Walker, R. G. (1984) Shelf and shallow marine sands. In Walker, R. G. (ed) Facies models, 2nd Edition. Geol. Assoc. Can., Waterloo, Ontario, 1-14. Walker, R. G. (1992) General Introduction: Facies Sequence and Facies Models. In Walker, R. G. and James, N. P. (eds) Facies Models: Response to Sea Level Change. Geol. Assoc. Can., Waterloo, Ontario, 1-14. Walker, R. G. (1992) Wave- and Storm-Dominated Shallow Marine Systems. In Walker, R. G. and James, N. P. (eds) Facies Models: Response to Sea Level Change. Geol. Assoc. Can., Waterloo, Ontario, 219-238. Walker, R. G., Duke, W. L. and Leckie, D. A. (1983) Hummocky stratification: Significance of its variable bedding sequences: Discussion. Geol. Soc. Am. Bull., 94, 1245-1249. Walker, R. G. and Plint, A. G. (1992) Wave- and storm-dominated shallow marine systems. In Walker, R. G. and James, N. P. (eds) Facies Models: Response to Sea Level Change. Geol. Assoc. Can., Waterloo, Ontario, 219-238. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/8843 | - |
dc.description.abstract | 高雄北部海岸平原區位屬台灣造山帶前緣之褶皺-逆衝斷層帶,前人在此地區以重力及反射震測調查,以及航照圖判識,判斷的構造有大灣向斜、岡山向斜、中洲背斜、半屏山背斜、小岡山斷層、右昌斷層和中洲斷層。本研究以中洲斷層及小岡山斷層將此區域劃分為四個構造區塊,由西向東分別為濱海平原區(大灣低地)、中洲台地(中洲背斜)、岡山低地(岡山向斜)及西部麓山帶。
為瞭解此區域褶皺-逆衝斷層帶之構造特性,本研究針對中央地調所在二仁溪以南之平原區鑽井17口,其中包含資源地質組在此區所鑽探之成功井等250公尺岩芯13口,以及構造與地震地質組針對小岡山斷層所鑽之四口岩芯(70~200公尺),重新做岩芯紀錄。透過沉積構造的判釋、岩相分類、岩相組合…等進行沉積環境及沉積層序的判釋。可得知末次冰期以來之沉積物厚度於各構造地形分區上相異之分布,及18,000年來海岸線的變遷和沉積環境的演化。 再藉由古環境沉積深度、碳十四定年年代、以及當時全球海水面變化高度,推估此區之地殼變動速率。結果顯示,濱海平原區為沉降區,平均沉降速率為-4.3±0.7 mm/yr;中洲台地(中洲背斜)為抬升區,其抬升速率從背斜軸部的3.0±0.9 mm/yr往兩翼遞減為-0.2±0.9 mm/yr;岡山低地(岡山向斜)為沉降區,沉降速率為-3.5±0.6 mm/yr;西部麓山帶前緣為抬升區,平均抬升速率為1.5±0.9 mm/yr。中洲斷層的活動導致中洲背斜的形成,其地下構造可能為斷層擴展褶皺的模式。小岡山斷層並未明顯的截穿覆蓋於其上之全新世沉積層,僅造成沉積層褶曲變形,根據其相異的抬升速率可將之分為南北兩段,小崗山斷層北段變形帶上垂直錯移速率>3.2±1.6 mm/yr,其淨滑移速率>4.0±2.3 mm/yr;而小崗山斷層南段的垂直錯移速率<5.0±1.5 mm/yr,淨滑移速率<6.1±2.4 mm/yr。 | zh_TW |
dc.description.abstract | The northern part of the Kaohsiung coastal-plain is an ongoing fold-and-thrust belt in the frontal orogenic belt. Previous studies concerning gravity and seismic profiles has shown that the structural framework in the study area is controlled by several NE trending thrust faults and folds, namely the Panpingshan anticline, Yuchang fault, Hsiaokangshan fault, Kangshan syncline, Chungchou anticline, Chungchou fault and Tawan syncline from east to west. The study aera can be divided into four tectonic domains by the Chungchou fault and the Hsiaokangshan fault ,including the coastal plain (Tawan syncline), the Chungchou tableland (Chungchou anticline), the Kangshan lowland (Kangshan syncline) and the western Foothills from west to east.
Based on the structural characteristics of the frontal fold-and-thrust belt, the borehole logging drilled by Central Geological Survey was rechecked in order to estimate the deformation rate through analysis of paleo-depositional environment, sequence stratigraphy, and radiocarbon dating. The result shows that subsidence rate of the Tawan syncline is -4.3±0.7 mm/yr, uplift rate of the Chungchou anticline is 3.0±0.9 mm/yr in axis and -0.2±0.9 mm/yr in limb, subsidence rate of the Kangshan syncline is -3.5±0.6 mm/yr, and uplift rate of the western Foothills is 1.5±0.9 mm/yr. The fault-propagation folding is proposed for which the Chungchou fault propagated and caused forming of the Chungchou anticline, and resulted into the Chungchou tableland. Hsiaokangshan fault deformed the overlying Holocene deposits but doesn’t cut the latter through. In addition, the Hsiaokangshan fault can be divided into two segments for different uplift rates, the northern segment has the vertical slip rate more than 3.2±1.6 mm/yr and its net slip rate probably more than 4.0±2.3 mm/yr, while the southern segment has the vertical slip rate less than 5.0±1.5 mm/yr and its net slip rate probably less than 6.1±2.4 mm/yr. | en |
dc.description.provenance | Made available in DSpace on 2021-05-20T20:02:26Z (GMT). No. of bitstreams: 1 ntu-98-R94224118-1.pdf: 42397579 bytes, checksum: d5d5702821cee65c4756736f129e050a (MD5) Previous issue date: 2009 | en |
dc.description.tableofcontents | 口試委員會審定書…………………………………………………… I
誌謝…………………………………………………………………… II 中文摘要……………………………………………………………… VI 英文摘要……………………………………………………………… V 目錄…………………………………………………………………… VI 圖目……………………………………………………………………VIII 表目…………………………………………………………………… X 第一章 緒論………………………………………………………… 1 1.1前言…………………………………………………………… 1 1.2地質背景……………………………………………………… 1 1.3研究方法……………………………………………………… 8 第二章 岩芯紀錄…………………………………………………… 9 2.1岩芯資料……………………………………………………… 9 2.2岩相分析……………………………………………………… 13 2.3岩相組合與沉積環境………………………………………… 19 第三章 沉積層序分析……………………………………………… 24 3.1層序界限……………………………………………………… 24 3.2體系域………………………………………………………… 25 3.3層序分析……………………………………………………… 28 3.4層序對比……………………………………………………… 32 第四章 地殼變動速率……………………………………………… 38 4.1地殼變動速率估算法………………………………………… 38 4.2末次冰期以來海水面變動…………………………………… 39 4.3高雄海岸平原區地殼變動速率……………………………… 40 第五章 討論………………………………………………………… 51 5.1高雄海岸平原區沉積層特性………………………………… 51 5.2地殼變動速率………………………………………………… 55 5.3高雄海岸平原區地下構造特性……………………………… 58 第六章 結論………………………………………………………… 61 參考文獻……………………………………………………………… 63 附錄…………………………………………………………………… 71 | |
dc.language.iso | zh-TW | |
dc.title | 高雄北部海岸平原區末次冰期沉積環境分析-探討褶皺-逆衝斷層帶前緣之滑移速率 | zh_TW |
dc.title | The Postglacial Marine Environment of the Northern Kaohsiung Coastal Plain-its implications for slip rate of the frontal fold-and-thrust belt | en |
dc.type | Thesis | |
dc.date.schoolyear | 97-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 林啟文,楊志成 | |
dc.subject.keyword | 小崗山斷層,斷層滑移速率,中洲斷層, | zh_TW |
dc.subject.keyword | Hsiaokangshan fault,Chungchou fault,fold-and-thrust belt,net slip rate, | en |
dc.relation.page | 108 | |
dc.rights.note | 同意授權(全球公開) | |
dc.date.accepted | 2009-08-19 | |
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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