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姓名	李慶蘭(Chin-Lan Lee)  查詢紙本館藏	畢業系所	地球物理研究所
論文名稱	苗栗白沙屯地區頭嵙山層之年代地層與沉積環境
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摘要(中)	本研究針對位於苗栗縣白沙屯地區之頭嵙山層，選擇七個剖面，利用鈣質超微化石及有孔蟲化石對本區域之地層做地質年代及沉積環境上的解析與比較。 依據鈣質超微化石之分析結果，白沙屯地區各剖面地質時代均屬於更新世早期，即Pseudoemiliania lacunosa帶中上部，絕對年代約為1.24~0.46Ma。各剖面中最老的磚場剖面（ZC）屬於small Gephyrocapsa亞帶，絕對年代為1.24~1.03Ma，最年輕的清海宮剖面（CHK）屬於Pseudoemiliania lacunosa亞帶末期，其他剖面屬於Pseudoemiliania lacunosa亞帶，絕對年代為1.03~0.46Ma。 由鈣質超微化石環境分析其沉積環境，各剖面因含有Helicosphaera, Coccolithus及Discolithina等種屬，指示地層之古沉積環境為開闊、近岸之淺海環境，本區域之浮游性有孔蟲化石群集亦以暖水域的種屬為主。 根據底棲性有孔蟲化石的環境分析結果，各剖面的層位稍有不同，除了磚場剖面（ZC）的底棲性有孔蟲化石之優勢種為Bolivina、Melonis、Textularia及Discorbis（B-M-T-D）群集，顯示的古沉積環境為正常鹽度、較深的中~外大陸棚環境外，其餘剖面之底棲性有孔蟲化石優勢種為Textularia、Cibicides、Quinqueloculina及Discorbis（T-C-Q-D）群集，顯示其古沉積環境為正常鹽度、較淺的內大陸棚環境。 依據過港貝化石層之浮游性有孔蟲化石碳氧同位素分析結果，顯示該沉積物沉積當時為更新世暖期，與底棲性有孔蟲化石、鈣質超微化石及浮游性有孔蟲化石分析之結果相符。
摘要(英)	Based on the calcareous nannofossil study, the geological age of the sections of Paishatung area is determined as early Pleistocene in age. They can be assigned to the middle~upper parts of the Pseudoemiliania lacunosa Zone which corresponds to the age interval of 1.24~0.46Ma. The eldest one is correlated to the small Gephyrocapsa subzone which corresponds to the age interval of 1.24~1.03Ma. The youngest one is determined to the upper Pseudoemiliania lacunosa subzone. Others are assigned to the Pseudoemiliania lacunosa subzone which corresponds to the age interval of 1.24~1.03Ma. According to the analyses of the paleoenvironments by calcareous nannofossils, because of the existing of the genus, Helicosphaera, Coccolithus and Discolithina, the paleosedimentary environment of the sections is open neritic-shallow marine. The dominated species of the planktonic foraminiferal fossils belongs to warm fauna. From the results of paleoenvironments analyses by the benthonic foraminiferal fossils, only one section belongs to the B-M-T-D assemblage composed mainly by Bolivina, Melonis, Textularia and Discorbis. The assemblage indicates the environment of middle~outer shelf with deeper and normal salinity water mass. Others belongs to the T-C-Q-D assemblage composed by Textularia, Cibicides, Quinqueloculina and Discorbis. The assemblage indicate the environment of inner shelf with shallower and normal salinity water mass. The results of carbon-oxygen isotopic composition from Koukang Shell Bed was suggested that they were deposited in a warm period of the Pleistocene. This conclusion agreed with the results of the analysis by planktonic and benthonic foraminiferal fossil and calcareous nannofossils.
關鍵字(中)	★ 底棲性有孔蟲化石 ★ 浮游性有孔蟲化石 ★ 鈣質超微化石 ★ 年代地層 ★ 沉積環境 ★ 白沙屯 ★ 頭嵙山層 ★ 過港貝化石層	關鍵字(英)	★ benthonic foraminifera ★ planktonic foraminifera ★ calcareous nannofossil ★ ronostratigraphy ★ sedimentary environment ★ Paishatung ★ Toukoshan formation ★ Koukang Shell Bed
論文目次	第一章 緒論1 1.1 研究目的1 1.2 前人研究2 1.2.1 地層2 1.2.2 生物地層與地質年代3 1.2.3 環境分析5 第二章 地形與區域地質7 2.1 位置與交通7 2.2 地形7 2.3 區域地質10 2.3.1 地層概述10 2.3.2 地質構造13 第三章 研究方法14 3.1 標本的採取14 3.1.1 野外地質調查與標本採集14 3.1.2 露頭剖面描述14 3.2 標本處理21 3.2.1 鈣質超微化石21 3.2.2 有孔蟲化石23 第四章 化石產狀25 4.1 清海宮剖面（CHK）25 4.1.1 有孔蟲化石25 4.1.2 鈣質超微化石35 4.2 赤土崎剖面（CTC）36 4.2.1 有孔蟲化石36 4.2.2 鈣質超微化石36 4.3 龍港剖面（LK）38 4.3.1 有孔蟲化石38 4.3.2 鈣質超微化石38 4.4 菜圃剖面（CB）39 4.4.1 有孔蟲化石39 4.4.2 鈣質超微化石39 4.5 拱天宮剖面（GTK）39 4.5.1 有孔蟲化石39 4.5.2 鈣質超微化石40 4.6 友愛靈園剖面（CMY）40 4.6.1 有孔蟲化石40 4.6.2 鈣質超微化石41 4.7 磚場剖面（ZC）41 4.7.1 有孔蟲化石41 4.7.2 鈣質超微化石42 4.8 結論42 第五章 年代地層45 5.1 鈣質超微化石45 5.1.1 Gephyrocapsa oceanic Kamptner47 5.1.2 Pseudoemiliania lacunosa（Kamptner）48 5.1.3 討論49 5.1.4 結論50 5.2 浮游性有孔蟲化石51 5.2.1 討論52 5.2.2 結論52 5.3 底棲性有孔蟲化石53 5.3.1 討論53 5.3.2 結論53 5.4 結論55 第六章 環境分析57 6.1 底棲性有孔蟲化石57 6.1.1 Murray模式57 6.1.2 討論69 6.1.3 結論76 6.2 浮游性有孔蟲化石76 6.2.1 討論80 6.2.2 結論83 6.3 鈣質超微化石86 6.3.1 討論與結論86 6.4 其他資料86 6.5 結論87 第七章 結論88 參考文獻90 附錄A 沉積柱狀圖與露頭照片98 附錄B 圖版 110 附錄C 底棲性有孔蟲化石分類表143
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指導教授	黃敦友	審核日期	2000-7-20
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