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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 宋聖榮 | |
dc.contributor.author | Chang-Chao Chang | en |
dc.contributor.author | 張阡肇 | zh_TW |
dc.date.accessioned | 2021-06-13T16:44:38Z | - |
dc.date.available | 2005-07-11 | |
dc.date.copyright | 2005-07-11 | |
dc.date.issued | 2005 | |
dc.date.submitted | 2005-06-29 | |
dc.identifier.citation | 參考文獻
中文部分 王鑫、徐美玲、楊建夫 (1988) 台灣泥火山地形景觀:台灣省立博物館年刊,第三十一卷,第31~49頁。 王士偉、戴昌鳳、宮守業 (2002) 非碳酸鹽環境中珊瑚礁的最初發育基底:國立台灣大學地質學系錢憲和教授羅煥記榮退研討會論文集,144~148頁。 王士偉、戴昌鳳、宮守業、米泓生 (2003) 臺灣西南地區更新世礁灰岩與基底泥岩的接觸關係:中國地質學會九十二年年會暨學術研討會論文摘要,第85頁。 中國石油公司台探總處 (1992) 高雄-屏東地質圖幅:中國石油股份有限公司台灣油礦探勘總處編印,中國測量工程協會印刷。 市川雄一(1927)台灣珊瑚石灰岩:地理學雜誌,第39卷,第462期,第441~444頁。 何春蓀(1975)台灣地質概論-台灣地質圖說明書:經濟部出版,153頁。 吳樂群、王源(1989)台灣嘉義地區澐水溪剖面上中新統至下更新統之沈積環境:地質,第九卷,第一期,第15~44頁。 吳樂群 (1993) 台灣南部旗山地區上部新第三系及第四系之沉積層序與演化:國立台灣大學地質學研究所博士論文,212頁。 吳榮章、梅文威(1992)高雄縣旗山至鳳山地區生物地層與古沈積環境研究:經濟部中央地質調查所特刊,第六號,第263~295頁。 吳天偉 (1999) 由沉積岩學及古生態學分析高雄半屏山石灰岩體之生成過程:國立台灣大學地質研究所碩士論文,183頁。 李妍慧 (1990) 高雄附近石灰岩區之超微化石生物地層、年代對比與古沉積環境研究:國立中山大學海洋地質研究所碩士論文,84頁。 李金祥(1996)琉球嶼海底泥火山之成因與震測解釋之研究:國立海洋大學應用地球物理研究所碩士論文,93頁。 李真瑩(2003)台灣西南部海域的泥貫入體與天然氣水合物的生成:國立海洋大學應用地球物理研究所碩士論文,79頁。 余輝龍、施輝煌、黃春盛、何智剛、曾寶樹(1990)台南縣龍船及高雄縣坑內小滾水構造重點地質核查報告:中油內部報告。 林殿順(1991)台灣西南部麓山帶上新-更新統之沈積岩相與沈積環境演化:國立台灣大學地質學研究所碩士論文,93頁。 林啓文、張徽正、盧詩丁、石同生、黃文正 (2000) 台灣活斷層概論-五十萬分之一台灣活動斷層分布圖說明書(第二版):經濟部中央地質調查所特刊,第十三號,122頁。 洪崇勝 (1991) 台灣西南部曾文溪、二仁溪剖面磁性礦物與磁地層之研究:國立台灣大學海洋研究所博士論文,324頁。 徐慶雲(1975)台南縣坑內、龍船及高雄縣小滾水構造地質核查報告:中油內部報告。 翁群評(2001)小崗山斷層及其附近構造:國立中央大學地球物理研究所碩士論文,84頁。 張錫齡(1962)六雙層之命名:中國地質學會專刊,第一號,第189~192頁。 張成華(1993)台灣西南部海域泥貫入體研究:國立台灣大學海洋研究所碩士論文,71頁。 張益生(1994)台灣西南部麓山帶上部中新統至更新統砂岩岩象與黏土礦物之分析及其構造意義:國立台灣大學地質科學研究所碩士論文,86頁。 曹恕中、李翠瓊、田蓉禮、陳肇夏、劉聰桂、陳正宏 (1992) 中部橫貫公路東段岩層伊來石結晶度與核飛跡年代分析:國立台灣大學理學院研究報告,第30期,第45~64頁。 陳華玟(1992)台灣南部高雄半屏山石灰岩地層層序及造礁作用與造礁生物之研究:經濟部中央地質調查所八十一年度年報,第41~43頁。 陳華玟、吳樂群、錢憲和 (1994) 台灣南部高雄地區早更新世半屏山石灰岩與古亭坑層的接觸關係:經濟部中央地質調查所特刊,第八號,第101~119頁。 陳華玟(1995)高雄地區早更新世石灰岩的地層層序研究:經濟部中央地質調查所八十三年度年報,第50~55頁。 陳華玟、吳樂群、錢憲和(1997)台灣南部高雄地區更新世石灰岩的層位及其成因:第四屆地層研討會-台灣西南部地區地質研討會大會手冊及論文摘要,第74~77頁。 陳華玟、謝凱旋、何信昌 (1998) 台灣地質圖幅說明書-高雄,圖幅第六十一號:經濟部中央地質調查所,47頁。 陳志雄、吳樂群、王源(1993)高雄地區旗山斷層兩側地層年代之檢討:地質,第十三卷,第一期,第37~56頁。 陳文山、何信昌、王源、楊昭男、高明健、張益生、鄂忠信、陳勉銘(1994)台灣西南部上新統至更新統的岩象學研究與地層對比:經濟部中央地質調查所特刊,第八號,第83~99頁。 陳儀清(1997)台灣西南外海海床表層沈積現象之研究:國立台灣大學海洋研究所博士論文,160頁。 黃立勝(1990)台灣西部晚新生代沈積盆地之地下溫度及地溫梯度之研究:經濟部中央地質調查所彙刊,第六號,第117-144頁。 黃鑑水、張憲卿、劉桓吉 (1994) 台灣南部觸口斷層之地質調查與探勘:經濟部中央地質調查所彙刊,第九號,第51~76頁。 黃偉倫(1995)台灣西南部海域泥貫入體之分部與陸上諸背斜之關係及其對沈積環境之影響:國立台灣大學海洋研究所碩士論文,68頁。 黃能偉(2001)台灣西南部更新統(左鎮地區)層序地層之初探:國立台灣大學地質科學研究所碩士論文,120頁。 詹博舜 (2001) 由穩定氫氧同位素探討台灣西南活動構造帶泉水之來源:國立台灣大學地質科學研究所碩士論文,80頁。 葉高華 (2003) 由流體地球化學探討台灣泥火山的成因:國立台灣大學海洋研究所碩士論文,61頁。 趙鴻樁(2003)台灣地區泥火山氣體成分分析及其對全球甲烷來源的可能影響:國立成功大學地球科學研究所碩士論文,81頁。 劉忠光、藍晶瑩、蘇強、恩斯特(1977)東台灣之蛇綠岩系(其產狀、岩石學、變質作用及構造背景之研究):礦業研究所特刊,第一號,212頁。 劉穎、劉海臣、李獻華(1996)用ICP-MS準確測定岩石樣品中的40餘種微量元素:地球化學,第25卷,第6期,第552~558頁。 鄭宏祺(2000)台灣西南部台南至屏東地區地質構造之研究:國立中央大學應用地質研究所碩士論文,92頁。 賴宗德(1996)台灣西南海域震測資料所顯示之新構造意義:國立海洋大學應用地球物理研究所碩士論文,66頁。 謝凱旋(1990)台南高雄泥岩區地質層序及生物地層研究:經濟部中央地質調查所未刊報告,第2頁。 謝佩珊 (2000) 台灣地區溫泉與泥火山氣體來源之初探:國立台灣大學地質科學研究所碩士論文,77頁。 謝孟龍、謝凱旋、李元希、陳政恆、楊志成、謝佳寧(2000)西南部泥岩區龍船斷層的構造特徵:中國地質學會八十九年年會大會手冊暨論文摘要,第322~323頁。 顏滄波、張麗旭(1949)台南關仔嶺枕頭山之石灰岩:台灣省地質調查所彙刊,第二號,第5~10頁。 英文部分 Aloisi, G.., Pierre, C., Rouchy, J. M., Foucher, J. P., Woodside, J., and the Medinaut Scientific Party, 2000. Methane-related authigenic carbonates of eastern Mediterranean Sea mud volcanoes and their possible relation to gas hydrate destabilization. Earth and Planetary Science Letters, 184, 321-338. Aloisi, G.., Pierre, C., Rouchy, J. M., and Faugeres, J. C., 2002. Isotopic evidence of methane-related diagenesis in the mud volcanic sediments of the Barbados Accretionary Prism. Continental Shelf Research, 22, 2355-2372. Awwiller, D. N., 1994. Geochronology and mass transfer in Gulf Coast mudrocks(south-central Texas, USA):Rb-Sr, Sm-Nd, and REE systematics. Chemical Geology, 116, 61-84. Baker, P. A., and Kastner, M., 1981. Constraints on the formation of sedimentary dolomite. Science, 213, 214-216. Barber, A. J., Tjokrosapoetro, S., and Charlton, T. R., 1986. Mud volcanos, shale diapirs, wrench faults, and mélanges in accretionary complexes, eastern Indonesia. The American Association of Petroleum Geologists Bulletin, 70, 11, 1729-1741. Barth, M. G., McDonough, W. F., and Rudnick, R. L., 2000. Tracking the budget of Nb and Ta in the continental crust. Chemical Geology, 165, 197-213. Bohrmann, G., Greinert, J., Suess, E., and Torres, M., 1998. Authigenic carbonates from the Cascadia subduction zone and their relation to gas hydrate stability. Geology, v. 26, no.7, 647-650. Brown, K. M., 1990. The nature and hydrogeologic significance of mud dirpirs and diatrems for accretionary systems. Journal of Geophysical Research, 95(B5), 8969-8982. Chang, L. S., 1967. A biostratigraphic study of the Tertiary in the Coastal Range, eastern Taiwan, based on smaller foraminifera. (I. Southern Part). Proceedings of the Geological Society of China, 10, 64-76. Chang, L. S., and Chi, W. R., 1983. Neogene nannoplankton biostratigraphy in Taiwan and the tectonic implications. Petroleum Geology of Taiwan, 19, 93-148. Chen, P. H., Huang, T. C., Huang, C. Y., and Tsai, L. P., 1977. A study of the late Neogene marine sediments of the Chinshan area, Taiwan: Paleomagnetic stratigraphy, biostratigraphy and paleoclimate. Memoir of the Geological Society of China, 2, 169-190. Chow, J., Lee, J.S., Sun, R., Liu, C.S., and Lundberg, N., 2000. Characteristics of the bottom simulating reflectors near mud diapirs. Geo-Marine Letters, 20, 3-9. Chow, J., Lee, J.S., Liu, C.S., Lee, B.D. and Watkins, J.S., 2001. A submarine canyon as the cause of a mud volcano-Liuchieuyu Island in Taiwan. Marine Geology, 176, 55-63. Chen, W. S., Ridgway, K. D., Horng, C. S., Chen, Y. G., Shea, K. S., and Yeh, M. G., 2001. Stratigraphic architecture, magnetostratigraphy, and incised-valley systems of the Pleocene-Pleistocene collisional marine foreland basin of Taiwan. Geological Society of America Bulletin, 113, 10, 1249-1271. Condie, K. C., 1993. Chemical composition and evolution of the upper continental crust: contrasting results from surface samples and shales. Chemical Geology, 104, 1-37. Cookenboo, H. O., and Bustin, R. M., 1999. Pore water evolution in sandstones of the Groundhog Coalfield, northern Bowser Basin, British Columbia. Sedimentary Geology, 123, 129-146. Cullers, R. L., Chandhuri, S., Arnold, B., Lee, M. and Wolf, C. W., 1975. Rare-earth distributions in clay minerals and clay-sized fractions of Lower Permian Havensville and Eskridge shales of Kansas and Oklahoma. Geochimica et Cosmochimica Acta, 39, 1691-1703. Cullers, R. L., Chandhuris, S., Kilbane, N., and Koch, R., 1979. Rare earths in size fractions and sedimentary rocks of Pennsylvanian-Permian age from the mid-continent of the U.S.A.. Geochimica et Cosmochimica Acta, 43, 1285-1302. Cullers, R. L., 1995. The controls on the major and trace element evolution of shales, siltstones and sandstones of Ordovician to Tertiary age in the Wet Mountains regions region, Colorado, U.S.A.. Chemical Geology, 123, 107-131. Davisson, M. L., Presser, T. S., and Criss, R. E., 1994. Geochemistry of tectonically expelled fluids from the northern Coast Range, Rumsey Hills, California, USA. Geochimica et Cosmochimica Acta, 58, 1687-1699. Dia, A. N., Castrec-Rouelle, M., Boulegue, J., and Comeau, P., 1999. Trinidad mud volcanoes: where do the expelled fluids come from?. Geochimica et Cosmochimica Acta, 63, 1023-1038. Dinelli, E., Lucchini, F., Mordenti, A., and Paganelli, L., 1999. Geochemistry of Oligocene-Miocene sandstones of the northern Apennines(Italy) and evolution of chemical features in relation to provenance changes. Sedimentary Geology, 127, 193-207. Faure, G., 1991. Principles and applications of inorganic geochemistry. Macmillan, New York, N. Y., 626. Feng, R., and Kerrich, R., 1990. Geochemistry of fine-grained clastic sediments in the Archean Abitibi greenstone belt, Canada: Implications for provenance and tectonic setting. Geochimica et Cosmochimica Acta, 54, 1061-1081. Fedo, C. M., Nesbitt, H. W., and Young, G. M., 1995. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance. Geology, 1995, 921-924. Fedo, C. M., Eriksson, K. A., and Krogstad, E. J., 1996. Geochemistry of shales from the Archean(~3.0Ga) Buhwa Greenstone Belt, Zimbabwe: Implication for provenance and source-area weathering. Geochimica et Cosmochimica Acta, 60, 10, 1751-1763. Fournier, R. O., and Rowe, J. J., 1966. Estimation of Underground Temperatures from the Silica Content of Water from Hot Springs and Wet-Steam Wells. American Journal of Science, 264, 685-697. Gieskes, J. M., You, C. F., Lee, T., Yui, T. F. and Chen, H. W., 1992. Hydro-geochemistry of mud volcanoes in Taiwan. Acta Geologica Taiwanica, 30, 79-88. Govindaraju, L., 1989. Geostandards Newsletter, Special Issue of Geostandards Newsletter. PP.28. Gong, S. Y., Lee, T. Y., Wu, J. C., Wang, S. W., and Yang, K. M., 1996. Possible links between the development of Plio-Pleistocene coral reef limestones and thrust migration in southwestern Taiwan. Journal of the Geological Society of China, 39, 2, 151-166. Gromet, L. P., Dymek, R. F., Haskin, L. A., and Korotev, R. L., 1984. The “North American Shale Composite”: its compilation, major and trace element characteristics. Geochimica et Cosmochimica Acta, 48, 2469-2482. Graue, K., 2000. Mud volcanoes in deepwater Nigeria. Marine and Petroleum Geology, 17, 959-974. Heim, A. and Chung, C. T., 1962. Preliminary observation on the structure of the Kaohsiung-limestone mountains. Petroleum Geology of Taiwan, 1, 23-30. Horng, C. S., and Shea, K. S., 1994. Study of nannofossil biostratigraphy in the eastern part of the Erhjenchi section, southwestern Taiwan. Special Publication of the Central Geological Survey, 8, 181-204. Hovland, M., Talbot, M. R., Qvale, H., Olaussen, S., and Aasberg, L., 1997. Methane-related carbonate cements in pockmarks of the North Sea. Journal of Sedimentary petrology, 57, 881-892. Hsu, C. Y., and Wey, S. K., 1983. Structural Geology in the Chiayi Foothills, Taiwan. Petroleum Geology of Taiwan, 19, 29-49. Huang, T. Y., 1969. Some planktonic foraminifera from a bore at Shihshan, near Taitung, Taiwan. Proceedings of the Geological Society of China, 12, 103-119. Huang, T. Y., 1977. Late Neogene planktonic foraminiferal biostratigraphy of the Tainan foothills region, Tainan, Taiwan. Petroleum Geology of Taiwan, 14, 121-145. Jahren, J. S., and Aagaard, P., 1989. Compositional variations in diagenetic chlorites and illites, and relationships with formation-water chemistry. Clay Minerals, 24, 157-170. Kastner, M., 1984. Control of dolomite formation. Nature, 311, 410-411. Kopf, A., and Deyhle, A., 2002. Back to the roots: boron geochemistry of mud volcanoes and its implications for mobilization depth and global B cycling. Chemical Geology, 192, 195-210. Lacombe, O., Angelier, J., Rocher, M., Chen, H. W., Chu, H. T., Deffontaines, B., Hu, J. C., and Lee, J. C., 1995. Calcite twin analysis: A key to the recent stress fields at the front of the Taiwan Collision belt, paper presented at International Conference and 3rd Sino-French Symposium on Active Collision in Taiwan, The Geological Society of China, Taipei, Taiwan, 157-166. Lacombe, O., Angelier, J., Chen, H. W., Deffontaines, B., Chu, H. T., and Rocher, M., 1997. Syndepositional tectonics and extension-compression relationships at the front of the Taiwan collision belt: A case study in the Pleistocene reefal limestones near Kaohsiung, SW Taiwan. Tectonophysics, 274, 83-96. Lacombe, O., Angelier, J., Mouthereau, F., Chu, H. T., Deffontaines, B., Lee, J. C., Rocher, M., Chen, R. F., and Siame, L., 2004. The Liuchiu Hsu island offshore SW Taiwan: tectonic versus diapiric anticline development and comparisons with onshore structures. Comptes Rendus Geoscience, 336, 815-825. Lee, C. Y., Ho, H. H., Chen, C. H., Yang, T. F., and Chung, S.L., 1996. Quantitative analysis of rocks samples by X-ray fluorescence: Journal of the Geological Society of China, v.39, no.3, 307-323. Lee, Y. I., 2002. Provenance derived from the geochemistry of late Paleozoic-early Mesozoic mudrocks of the Pyeongan Supergroup, Korea. Sedimentary Geology, 149, 219-235. Lin, S. B., and Hsueh, C. M., 1979. Clay mineralogy of Pliocene-Pleistocene sedimentary rocks in the foothill region east of Lungtien, southern Taiwan. Acta Geologica Taiwanica, 20, 109-128. Liu, C. S., Huang, I. L., and Teng, L. S., 1997. Structure features off southwestern Taiwan. Marine Geology, 137, 305-319. Li, X. H., Wei, G. J., Shao, L., Liu, Y., Liang, X., Jian, Z. M., Sun, M., and Wang, P. X., 2003. Geochemical and Nd isotopic variations in sediments of the South China Sea: a response to Cenozoic tectonism in SE Asia. Earth and Planetary Science Letters, 211, 207-220. Ludmann, T., and Wong, H. K., 2003. Characteristics of gas hydrate occurrences associated with mud diapirism and gas escape structures in the northwestern Sea of Okhotsk. Marine Geology, 201, 269-286. Matsumoto, R., 1990. Vuggy carbonate crust formed by hydrocarbon seepage on the continental shelf of Baffin Island, northeast Canada. Geochemical Journal, 24, 143-158. Martin, J. B., Kastner, M., Henry, P., Le Pichon, X., and Lallement, S., 1996. Chemical and isotopic evidence for sources of fluids in a mud volcano field seaward of the Barbados accretionary wedge. Journal of Geophysical Research, 101(B9), 20325-20345. McLennan, S. M., Nancy, W. B., and Taylor, R., 1980. Rare earth element-thorium correlations in sedimentary rocks, and the composition of the continental crust. Geochimica et Cosmochimica Acta, 44, 1833-1839. McLennan, S. M., Taylor, S. R., and Eriksson, K. A., 1983. Geochemistry of Archean shale from the Pilbara Supergroup, Western Australia. Geochimica et Cosmochimica Acta, 47, 1211-1222. McLennan, S. M., 1989. Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes. In: Lipin B. R. and McKay G. A. (Eds.), Review in Mineralogy, 21, 169-200. McLennan, S. M., and Taylor, S. R., 1991. Sedimentary rocks and crustal evolution: tectonic setting and secular trends. The Journal of Geology, 99, 1-21. McLennan, S. M., Hemming, S., McDaniel, D. K., and Hanson, G. N., 1993. Geochemical approaches to sedimentation, provenance and tectonics. In: Johnsson, M. J., Basu, A. (Eds.), Processes Controlling the Composition of Clastic Sediments. Geological Society of America, Boulder, CO, 21-40. Meisel, T., Koeberl, C., and Ford, R. J., 1990. Geochemistry of Darwin impact glass and target rocks. Geochimica et Cosmochimica Acta, 54, 1463-1474. Nesbitt, H. W., Markovics, G., and Price R. C., 1980. Chemical processes affecting alkalis and alkali earths during continental weathering. Geochimca et Cosmochimica Acta, 44, 1659-1666. Nesbitt, H. W. and Young, G. M., 1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299, 715-717. Nyakairu, G. W. A. and Koeberl, C., 2001. Mineralogical and chemical composition and distribution of rare earth elements in clay-rich sediments from central Uganda. Geochemical Journal, 35, 13-28. Pan, Y. S., 1968. Interpretation and seismic coordination of the Bouguer anomalies obtained in southwestern Taiwan. Petroleum Geology of Taiwan, 6, 197-208. Piper, D. Z., 1973. Origin of metalliferous sediments from the east pacific rise. Earth and Planetary Science Letters, 19, 75-82. Pierre, C., Rouchy, J. M., and Gaudichet, A., 2000. Diagenesis in the gas hydrate sediments of the Blake Ridge. Mineralogy and stable isotope compositions of the carbonate and sulphide minerals, in: Paull, C. K., Matsumoto, R., Wallace, P. J., Dillon, W. P. (Eds.). Proceedings of the ODP, Scientific Results, 164, 139-146. Reed, D., Lundberg, N., Liu, C. S., and Kuo, B. Y., 1992. Structural relations along the margins of the offshore Taiwan accretionary wedge: implication for accretion and crustal kinematics. Acta Geologica Taiwanica, 30, 105-122. Ritger, S., Caeson, B., and Suess, E., 1987. Methane-derived authigenic carbonates formed by subduction-induced pore-water expulsion along the Oregon/Washington margin. Geological Society of America Bulletin, 98, 147-156. Roser, B. P., and Korsch, R. J., 1986. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. The Journal of Geology, 94, 635-650. Roser, B. P., and Korsch, R. J., 1988. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data. Chemical Geology, 67, 119-139. Rocher, M., Lacombe, O., Angelier, J. and Chen, H. W., 1996. Mechanical twin sets in calcite as markers of recent collisional events in a fold-and –thrust belt: Evidence from the reefal limestones of southwestern Taiwan. Tectonics, 15, 5, 984-996. Shih, T. T., 1967. A survey of the active mud volcanoes in Taiwan and a study of their types and character of the mud. Petroleum Geology of Taiwan, 5, 259-311. Stach, L. W., 1957. Stratigraphic subdivision and correlation of the upper Cenozoic sequence in the foothills region east of Chiayi and Hsinying, Taiwan. Symposium on Petroleum Geology of Taiwan, 1956, 177-230. Stakes, D. S., Orange, D., Paduan, J. B., Salamy, K. A., and Maher, N., 1999. Cold-seeps and authigenic carbonate formation in Monterey Bay, California. Marine Geology, 159, 93-109. Sun, S. C., 1963. The reef limestone and the geologic structures in the vicinity of Kaohsiung City, Taiwan. Petroleum Geology of Taiwan, 2, 47-64. Sun, S. C., 1964. Photogeologic study of the Tainan-Kaohsiung coastal plain area, Taiwan. Petroleum Geology of Taiwan, 3, 35-51. Sun, S. C., 1965. On the occurrence of an uncomformity in the Upper Miocene Wushan Formation and Kaitzuliao Shale near Shengshuitsun, Kaohsiung, Taiwan. Proceedings of the Geological Society of China, 8, 100-102. Sun, S. C., and Liu, C. S., 1993. Mud diapers and submarine channel deposits in offshore Kaohsiung-Hengchun, Southwest Taiwan. Petroleum Geology of Taiwan, 28, 1-14. Swanberg, C. A., and Morgan, P., 1979. The linear relation between temperatures based on the silica content of groundwater and regional heat flow: A new heat flow map of the United States. Pure and applied geophysics, 117, 227-241. Taylor, S. R., and McLennan, S. H., 1981. The composition and evolution of the continental crust: rare earth element evidence from sedimentary rocks. Philosophical transactions of the Royal Society of London, A301, 381-399. Taylor, S. R., and McLennan, S. H., 1985. The continental crust: Its composition and evolution. Blackwell, Oxford, 312. Taylor, M. H., Dillon, W. P., and Pecher, I A., 2000. Trapping and migration of methane associated with the gas hydrate stability zone at the Blake Ridge Diapir: new insights from seismic data. Marine Geology, 164, 79-89. Vital, H., and Stattegger, K., 2000. Major and trace elements of stream sediments from the lowermost Amazon River. Chemical Geology, 168, 151-168. Vogt, P. R., Cherkashev, G., Ginsburg, G., Ivanov, G., Milkov, A., Crane, K., Lein, A., Sundvor, E., Pimenov, N., and Egorov, A., 1997. Haakon Mosby mud volcano provides unusual example of venting. EOS, 78, 540. Whiticar, M. J., and Faber, E., 1986. Methane oxidation in sediment and water column environments-Isotope evidence. Organic Geochemistry, 10, 759-768. Wronkiewicz, D. J., and Condie, K. C., 1987. Geochemistry of Archean shales from the Witwatersrand Supergroup, South Africa: Source-area weathering and provenance. Geochimica et Cosmochimica Acta, 51, 2401-2416. Wronkiewicz, D. J., and Condie, K. C., 1990. Geochemistry and mineralogy of sediments from the Ventersdorp and Transvaal Supergroups, South Africa: cratonic evolution during the early Proterozoic. Geochimica et Cosmochemica Acta, 54, 343-354. Yang, T. F., 2002. 3He/4He ratios of fluid samples in Taiwan. Geochimica et Cosmochimica Acta, 66, A859. Yang, T. F., Chen, C. H., Tien, R. L., Song, S. R., and Liu, T. K., 2003. Remnant magmatic activity in the Coastal Range of East Taiwan after arc-continent collision: fission-track date and 3He/4He ratio evidence. Radiation Measurements, 36, 343-349. Yang, T. F., Yeh, G. H., Fu, C. C., Wang, C. C., Lan, D. F., Lee, H. F., Chen, C. H., Walia, V., and Sung, Q. C., 2004. Composition and exhalation flux of gases from mud volcanoes in Taiwan. Environment Geology, 46, 1003-1011. You, C. F., Gieskes, J. M., Lee, T., Yui, T. F. and Chen, H. W., 2004. Geochemistry of mud volcano fluids in the Taiwan accretionary prism. Applied Geochemistry, 19, 695-707. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/38750 | - |
dc.description.abstract | 摘要
台灣陸地上有許多泥火山,大多坐落於西南部的海岸平原和麓山帶,以及東部海岸山脈南段利吉層泥岩中。由於泥火山沉積物可以紀錄整個泥火山作用的過程且與下覆岩石地層有密不可分的關係,為了區辨沈積物的來源,本研究採集了陸上泥火山沈積物及其附近地層岩樣來進行沈積物粒度、黏土礦物和地球化學的分析,藉由分析結果的比對,以探討泥火山沈積物的可能來源地層。此外,有越來越多的研究結果顯示甲烷源自生性碳酸鹽的沈澱都發生在海底泥火山的表面,因此,究竟有哪些證據支持泥火山的模式,也是本研究的另一研究目的。 研究結果顯示,主要元素的哈克圖中,鋁對其他元素的投影圖呈現線性關係,這可能是受到顆粒效應影響所造成的稀釋結果。經過標準化後,獲得兩個群體的分佈,且各對比於研究區域中之南部和北部,再由主要元素和微量元素的探討,且配合沈積物粒度的比較,推測下段古亭坑層為研究區域南部泥火山沈積物的主要來源,而中崙、關子嶺地區,由於中崙層與鳥嘴層化學性質相近,藉由二氧化矽地質溫度計的計算後,推測沈積物來源可能源自於中崙層。 另外,藉由Rb/Sr、Rb×100/Ti、Al/Ti、Ba/Nb比值增加和Th/La比值降低的變化與板岩岩屑含量增加一致,但西南部所有泥火山沈積物中的元素比值皆低於含板岩岩屑的地層-上部古亭坑層和下部古亭坑層的上部,推測泥火山沈積物主要來自於下部古亭坑層或更老地層,其深度至少深於1000公尺以上,然而也藉由這些比值的變化,推測板岩出露地層的年代為早期更新世。 綜合小崗山的斷層型態、碳同位素、泥岩礫堆積、石灰岩體中的二次化石以及在西南外海的琉球嶼泥火山發育更可當為現今陸上石灰岩體的類比,顯示台灣西南部的石灰岩體應該生長於古構造高區上,而此古構造高區可能就是泥火山或是泥貫入體。 | zh_TW |
dc.description.abstract | Abstract
Mud volcanoes are widely distributed in the southwest foothill, plain and eastern Coastal Range of Taiwan, as well as in many locations around the world. Generally, mud volcanoes are thought to be the expulsion of fluid from overpressurized sediments. Thus, the sediments can record the processes of mud volcanism and intimately associated with the beneath sedimentary sequences. For better understanding about the sediment provenance of mud volcanoes, we have collected the samples from the mud volcanoes and sedimentary sequences in the southwest Taiwan and eastern Lichi Formation to study their particle sizes, clay minerals and geochemistry. In addition, there are growing results that methane-derived authigenic carbonate precipitation occurs on surface mud volcanoes. The aims of this article are to correlate their provenance and to develop a model for origin of coral reefs through summarizing the previous studies and our data. Several results have been drawn from the present study: (1) variation diagrams of major elements show linear trends owing to grain-size effect. After normalization, there are two distinct groups over the southwest Taiwan. One group is located in the northern part while another in the southern part; (2) the lower Gutingkeng Formation in the southern part should be the main source in terms of geochemical and particle size data; (3) the sediments of Chunglung and Kuantzuling hot springs may be originated from Chunglung Formation based on estimation of silica geothermometer and geochemical data; (4) increase in Rb/Sr, Rb×100/Ti, Al/Ti, and Ba/Nb ratios and a decrease in the Th/La ratio of the Kanhsialiao Formation beginning at early Pleistocene are consistent with input of slates in the source region. However, all mud volcano sediments show low values in these ratios and suggest that the source sediments may be derived from more than 1 km depth; (5) fault characteristics, carbon isotope data, mud breccia, reworked fossils, and analogue of Liuchieuyu mud volcano, indicate that the limestones in the southwest Taiwan may develop at local structural highs where mud volcanoes occurred. | en |
dc.description.provenance | Made available in DSpace on 2021-06-13T16:44:38Z (GMT). No. of bitstreams: 1 ntu-94-R91224101-1.pdf: 3443547 bytes, checksum: 4966bc3c5baacd4a63c88f75cf534407 (MD5) Previous issue date: 2005 | en |
dc.description.tableofcontents | 目錄
致謝…………………………………………………………………Ⅰ 摘要…………………………………………………………………Ⅱ 目錄…………………………………………………………………Ⅳ 圖目錄………………………………………………………………Ⅶ 表目錄………………………………………………………………Ⅹ 第一章 緒論 1-1 前言………………………………………………… 1 1-2 前人研究. 1-2-1 陸上泥火山研究…………………………… 2 1-2-2 西南部石灰岩體研究……………………… 4 1-2-3 甲烷源自生性碳酸鹽研究………………… 6 1-3 研究目的…………………………………………… 7 第二章 研究區域概況 2-1 區域地質背景……………………………………… 8 2-1-1岩石地層 ……………………………………18 2-1-2主要斷層 ……………………………………23 2-1-3主要褶皺 ……………………………………25 2-2 採樣地點 2-2-1 岩層採樣……………………………………25 2-2-2 泥火山沈積物採樣 2-2-2-1 觸口斷層區……………………… 29 2-2-2-2 高屏海岸平原區………………… 29 2-2-2-3 旗山斷層區……………………… 29 2-2-2-4 古亭坑地區 ………………………31 2-2-2-5 海岸山脈區……………………… 31 2-2-3石灰岩體與泥接觸面採樣………………… 31 第三章 研究方法 3-1 研究材料 ………………………………………… 33 3-2 沉積物粒徑分析 ………………………………… 33 3-3 黏土礦物學分析 ………………………………… 33 3-4 岩象學分析 ……………………………………… 35 3-5 全岩地球化學分析 3-5-1 沉積物顆粒化學元素半定量分析 ……… 36 3-5-2 燒失量分析 ……………………………… 36 3-5-3 主要元素分析 …………………………… 36 3-5-4 微量元素與稀土元素分析 ……………… 37 第四章 分析結果 4.1 沉積物粒徑分析結果 …………………………… 38 4.2 黏土礦物半定量分析結果 ……………………… 45 4.3 岩象觀察結果 …………………………………… 47 4.4 沉積物顆粒化學元素半定量結果 ……………… 49 4.5 主要元素分析結果 ……………………………… 50 4.6 微量元素分析結果 ……………………………… 61 第五章 綜合討論 5.1 泥火山沉積物的地球化學特徵 ………………… 71 5.2 泥火山沈積物的可能來源地層 ………………… 74 5.3 影響泥火山沈積物來源的因數 ………………… 79 5.4 沈積物可能來源深度 …………………………… 86 5.5 板岩出露地層的年代 …………………………… 89 5.6 東部泥火山有無鈉長石化 ……………………… 90 5.7 西南部石灰岩體的起源 ………………………… 91 第六章 結論 …………………………………………………… 95 參考文獻 ……………………………………………………… 97 | |
dc.language.iso | zh-TW | |
dc.title | 台灣泥火山沈積物之特性、來源與西南部石灰岩體之隱示 | zh_TW |
dc.title | Characteristics and Source of Mud Volcano Sediments and Its Implication | en |
dc.type | Thesis | |
dc.date.schoolyear | 93-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 楊燦堯,陳汝勤,王詠絢 | |
dc.subject.keyword | 泥火山, | zh_TW |
dc.subject.keyword | Mud Volcano, | en |
dc.relation.page | 111 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2005-06-30 | |
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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