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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳文山(Wen-Shen, Chen) | |
| dc.contributor.author | Tsung-Jen Wu | en |
| dc.contributor.author | 吳琮壬 | zh_TW |
| dc.date.accessioned | 2021-06-13T00:02:03Z | - |
| dc.date.available | 2007-07-31 | |
| dc.date.copyright | 2007-07-31 | |
| dc.date.issued | 2007 | |
| dc.date.submitted | 2007-07-31 | |
| dc.identifier.citation | 中文部分
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/28169 | - |
| dc.description.abstract | 本研究區域北以朴子溪為界，南至曾文溪流域北段，東緣與西部麓山帶前緣為鄰，西緣連接台灣海峽，主要在嘉義縣、市以及台南縣的範圍之內。利用民國87 年至92 年，中央地質調查所於嘉義地區的18 口鑽探岩心為研究主體。先就各種岩性以及特徵，將其分類為14 個岩相－1 個礫岩相、7 個砂岩相、1 個砂泥岩互層相以及5 個泥岩相。並藉由砂質沉積物組成分析建立三種分類：Type 1、Type 2 以及Type 3，用以辨識沉積物來源，並輔助岩相組合來解釋沉積物是否受沿岸流作用的影響。
本研究利用岩相特徵並參考現生環境建立沉積模型，認為此區域在末次冰期以來具有二種沉積體系：曲流河作用與潮汐（或包括沿岸流作用）作用。各沉積體系可細分以下9 種次環境：曲流河相、河口砂洲相、沼澤相、潮坪相、潮汐水道、潟湖相、沿岸砂洲相、潮下帶相以及遠濱過度帶相。藉由層序分析，推論出末次冰期時，研究區域出露地表，接受風化與侵蝕作用形成土壤層，同時造成古八掌溪的遷移與下切，形成二個下切河谷。藉由剖面對比，建立本研究區域的沉積史。 約18000年前，全區域出露地表，形 成土壤層與下切河谷。約14000年前，海水面逐漸上升，在二個下切河谷形成江灣。 約12000－11000年前由於受到新仙女木亞冰期影響，環境略微淺化，海岸線向海側 遷移。約8000年前，海水已經覆蓋全區域，並入侵至西部麓山帶前緣。約5000年前， 沉積環境逐漸變淺。海岸線向海側遷移。5000年前至今，沉積物持續大量朝海側堆 積，海岸線位置持續向海側遷移。約400年前古籍記錄當時平原區呈現數個內海，之 後因人為開發造成內海快速淤積，海岸後退至今日的位置。 | zh_TW |
| dc.description.abstract | The study used 18 cored boreholes in Chiayi coastal plain which were provided by the Central Geological Survey. Based on the grain size, sedimentary textures and bioturbation,
it can be divided into fifteen lithofacies. The sediment composition was classified into three types of Type 1, Type 2, and Type 3, and explaining that the sediments were formed by the longshore current and fluvial processes. Based on the modern environment of the coast, it can be subdivided nine environments of meander river, river mouth bar, marsh, tidal flat, tidal channel, lagoon, longshore bar, subtidal and offshore transition zones. Based on the depositional environment analysis and radiocarbon dating data, wedescript five stages of depositional environment during the late Pleistocene - Holocene. (1) Before 18000 yr BP (the last glacial epoch) : This area formed a subaerial environment and developed two incised valleys. (2) During 14000 yr BP: Due to the sea-level rising, the shoreline was migrated to the eastward, and the incised valley was formed a drowned valley. (3) During 12000-11000 yr BP (the Younger Dryas event): The sea-level rising rate is slightly slow. The shoreline was migrated eastward to the frontal foothills. (4) During 8000 yr BP: The maximum marine flooding stage was formed at 8000 – 8500 yr BP. The shoreline was still at frontal foothills. (5) During 5000 yr BP: The sediments continuously progradated to the seaward, hence, the shoreline was retreated and migrated to the westward. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-13T00:02:03Z (GMT). No. of bitstreams: 1 ntu-96-R91224110-1.pdf: 39285447 bytes, checksum: 5cbee590eacabd9595954692cd5268b3 (MD5) Previous issue date: 2007 | en |
| dc.description.tableofcontents | 目 錄
論文口試委員審定書 ------------------------------------------------------------------------ I 致謝 --------------------------------------------------------------------------------------------- II 中文摘要 --------------------------------------------------------------------------------------- III 英文摘要 --------------------------------------------------------------------------------------- IV 目錄 --------------------------------------------------------------------------------------------- V 圖目 --------------------------------------------------------------------------------------------- VII 表目 --------------------------------------------------------------------------------------------- X 第一章 前言 ----------------------------------------------------------------------------------- 1 1-1 研究動機 ----------------------------------------------------------------------------1 1-2 區域概況 ----------------------------------------------------------------------------1 1-3 研究材料 ----------------------------------------------------------------------------3 1-4 研究方法 ----------------------------------------------------------------------------6 第二章 沉積物組成與岩相學分析 --------------------------------------------------------9 2-1 沉積物組成分析 -------------------------------------------------------------------9 2-2 沉積物組成分析結果 ------------------------------------------------------------11 2-3 岩相學分析 -------------------------------------------------------------------------17 第三章 岩相組合與沉積環境 --------------------------------------------------------------23 3-1 沉積環境與岩相組合 ------------------------------------------------------------- 25 第四章 層序分析 -----------------------------------------------------------------------------35 4-1 層序地層 ---------------------------------------------------------------------------- 35 4-2 層序分析結果 ----------------------------------------------------------------------40 第五章 綜合分析與討論 --------------------------------------------------------------------64 5-1 定年資料 ----------------------------------------------------------------------------64 5-2 剖面對比 ----------------------------------------------------------------------------66 5-3 末次冰期以來嘉義地區古沉積環境的演化 ----------------------------------....79 第六章 結論 -----------------------------------------------------------------------------------84 VI 參考文獻 --------------------------------------------------------------------------------------- 86 附錄（一）--------------------------------------------------------------------------------------94 沉積相分析結果 ------------------------------------------------------------------------ 113 附錄（二） ------------------------------------------------------------------------------------- 168 圖版 ----------------------------------------------------------------------------------------------169 VII 圖 目 圖1-1 台灣的板塊構造立體圖 -------------------------------------------------------------2 圖1-2 研究區域主要河流流域地質圖 ----------------------------------------------------4 圖1-3 研究區域岩心井位分布圖 ----------------------------------------------------------5 圖1-4 研究流程圖 ----------------------------------------------------------------------------7 圖2-1 砂質沉積物組成分類 ----------------------------------------------------------------15 圖2-2 砂質沉積物組成Q – Ms - Sl三角成分圖 -----------------------------------------16 圖2-3 岩相分類 -------------------------------------------------------------------------------18 圖3-1 環境示意圖 ----------------------------------------------------------------------------24 圖3-2 圖例 -------------------------------------------------------------------------------------32 圖3-3 曲流河相示意地層柱 ----------------------------------------------------------------33 圖3-4 河口砂洲相示意地層柱 -------------------------------------------------------------33 圖3-5 沼澤相示意地層柱 -------------------------------------------------------------------33 圖3-6 潟湖相示意地層柱 -------------------------------------------------------------------33 圖3-7 潮坪相示意地層柱 -------------------------------------------------------------------33 圖3-8 潮汐水道相示意地層柱 -------------------------------------------------------------34 圖3-9 河口砂洲相示意地層柱 -------------------------------------------------------------34 圖3-10 潮下帶相示意地層柱 ---------------------------------------------------------------34 圖3-11 遠濱過渡帶相示意地層柱 ---------------------------------------------------------34 圖4-1 沉積空間變化示意圖 ----------------------------------------------------------------35 圖4-2 一次海水面變化之完整層序示意圖 ----------------------------------------------37 圖例 ---------------------------------------------------------------------------------------------47 圖4-3 港墘井層序分析分析結果 ----------------------------------------------------------48 圖4-4 過溝井層序分析分析結果 ----------------------------------------------------------49 圖4-5 馬稠後井層序分析分析結果 -------------------------------------------------------50 圖4-6 南靖井層序分析分析結果 ----------------------------------------------------------51 圖4-7 松梅井層序分析分析結果 ----------------------------------------------------------52 VIII 圖4-8 鹿草井層序分析分析結果 ----------------------------------------------------------53 圖4-9 布袋井層序分析分析結果 ----------------------------------------------------------54 圖4-10 新塭井層序分析分析結果 --------------------------------------------------------55 圖4-11 岸內井層序分析分析結果 --------------------------------------------------------56 圖4-12 新東井層序分析分析結果 --------------------------------------------------------57 圖4-13 白河井層序分析分析結果 --------------------------------------------------------58 圖4-14 錦湖井層序分析分析結果 --------------------------------------------------------59 圖4-15 文山井層序分析分析結果 --------------------------------------------------------60 圖4-16 新生井層序分析分析結果 --------------------------------------------------------61 圖4-17 重溪井層序分析分析結果 --------------------------------------------------------62 圖4-18 六甲井層序分析分析結果 --------------------------------------------------------63 圖5-1 末次冰期以來海水面變化示意圖 -----------------------------------------------67 圖5-2 港墘-過溝-布袋-新塭-錦湖-文山 剖面 ------------------------------------------74 圖5-3 馬稠後-松梅-岸內-新生 剖面 -----------------------------------------------------75 圖5-4 嘉義-南靖-永安-白河-重溪-六甲 剖面 ------------------------------------------76 圖5-5 過溝-松梅-馬稠後-鹿草-南靖-嘉義 剖面 ---------------------------------------77 圖5-6 錦湖-岸內-新東-永安 剖面 --------------------------------------------------------78 圖5-7 18000年前，末次冰期最盛時期嘉義地區古沉積環境示意圖 ---------------80 圖5-8 14000年前嘉義地區古沉積環境示意圖 ------------------------------------------80 圖5-9 12000-11000年前嘉義地區古沉積環境示意圖 ----------------------------------81 圖5-10 8000年前嘉義地區古沉積環境示意圖 ------------------------------------------81 圖5-11 5000年前嘉義地區古沉積環境示意圖 ------------------------------------------82 圖例 ---------------------------------------------------------------------------------------------95 港墘井岩性地層柱與沉積相地層柱 ------------------------------------------------------96 過溝井岩性地層柱與沉積相地層柱 ------------------------------------------------------97 馬稠後井岩性地層柱與沉積相地層柱 ---------------------------------------------------98 南靖井岩性地層柱與沉積相地層柱 ------------------------------------------------------99 松梅井岩性地層柱與沉積相地層柱 ------------------------------------------------------100 鹿草井岩性地層柱與沉積相地層柱 ------------------------------------------------------101 布袋井岩性地層柱與沉積相地層柱 ------------------------------------------------------102 IX 新塭井岩性地層柱與沉積相地層柱 ------------------------------------------------------103 岸內井岩性地層柱與沉積相地層柱 ------------------------------------------------------104 新東井岩性地層柱與沉積相地層柱 ------------------------------------------------------105 白河井岩性地層柱與沉積相地層柱 ------------------------------------------------------106 錦湖井岩性地層柱與沉積相地層柱 ------------------------------------------------------107 嘉義井岩性地層柱與沉積相地層柱 ------------------------------------------------------108 永安井岩性地層柱與沉積相地層柱 ------------------------------------------------------108 文山井岩性地層柱與沉積相地層柱 ------------------------------------------------------109 新生井岩性地層柱與沉積相地層柱 ------------------------------------------------------110 重溪井岩性地層柱與沉積相地層柱 ------------------------------------------------------111 六甲井岩性地層柱與沉積相地層柱 -------------------------------------------------------112 X 表 目 表1-1 鑽井岩心基資料 --------------------------------------------------------------------- 5 表2-1 砂岩薄片計量結果 ------------------------------------------------------------------ 12 表2-2 岩相分類簡表 ------------------------------------------------------------------------ 17 表3-1 沉積環境及其相關岩相組合分類簡表 ------------------------------------------ 23 表5-1 研究區域各岩心之定年資料 ------------------------------------------------------ 64 | |
| dc.language.iso | zh-TW | |
| dc.title | 嘉義海岸平原區末次冰期以來古沉積環境之研究 | zh_TW |
| dc.title | Sedimentary Environment of the Chiayi Coastal Plain
Since the Last Glacial Epoch | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 95-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 吳樂群(Leh-Chyun Wu),洪奕星(Eason Hong),游能悌(Neng-Ti Yu) | |
| dc.subject.keyword | 嘉義,海岸平原,沉積環境,末次冰期,環境變遷, | zh_TW |
| dc.subject.keyword | Chiayi,coastal plain,depositional environment,the last glacial epoch, | en |
| dc.relation.page | 186 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2007-07-31 | |
| 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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