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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 蘇志杰 | |
| dc.contributor.author | Chih-Jui Cheng | en |
| dc.contributor.author | 鄭智睿 | zh_TW |
| dc.date.accessioned | 2021-05-20T20:22:00Z | - |
| dc.date.available | 2009-02-10 | |
| dc.date.available | 2021-05-20T20:22:00Z | - |
| dc.date.copyright | 2009-02-10 | |
| dc.date.issued | 2008 | |
| dc.date.submitted | 2009-01-30 | |
| dc.identifier.citation | 中文部份
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Hung (1999) Geochemical and carbon isotopic characterization of particles collected in sediment traps from the East China Sea continental slope and the Okinawa Trough northeast of Taiwan. Continental Shelf Research, 19, 183-203. Song, G.. S. and Y. C. Chang (1993) Comment on “naming of the submarine canyons off northeastern Taiwan: A note”. Acta Oceanographica Taiwanica, 30, 77-84. Steinke, S., Y. J. J. Hanebuth, C. Vogt and K. Stattegger (2008) Sea level induced variations in clay mineral composition in the southwestern South China Sea over the past 17000 yr. Marine Geology, 250, 199-210. Tang, T. Y., J. H. Tai and Y. J.Yang (2000) The flow pattern north of Taiean and the migration of Kuroshio. Continental Shelf Research, 20, 349-371. Tang, T. Y., Y. Hsueh, Y. J. Yang, and J. C. Ma, (1998) Continental slope flow northeast of Taiwan. Journal of Physical Oceanography, 29, 1353-1362. Uyeda, S. and H. Kanamori (1979) Back-arc opening and the model of subduction. Journal of Geophysical Research, 84, 1049-1061. Yu, H. S. and E. Hong (1992) Physiographic characteristics of the continental margin, northeast Taiwan. Terrestrial, Atmospheric and Oceanic Sciences, 3, 419-434. 網頁資料 Phil Jeffrey (2006) X-ray Data Collection Course. http://xray0.princeton.edu/~phil/Facility/Guides/XrayDataCollection.html Poppe, L. J., V. F. Paskevich, J. C. Hathaway, and D. S. Blackwood (2001) A Laboratory Manual for X-Ray Powder Diffraction. http://pubs.usgs.gov/of/of01-041/index.htm. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/9425 | - |
| dc.description.abstract | 黏土礦物在海洋研究中普遍被用來當作沈積物的來源與傳輸的指標，沈積物中黏土礦物的種類及分布情形與鄰近區域岩石源區的性質和氣候有關。本研究依照美國地質調查所（USGS）所公布之黏土礦物分析方法流程，使用X光繞射法（X-Ray Diffraction; XRD）鑑定黏土礦物種類並進行半定量分析工作。
研究結果顯示，南沖繩海槽表層沈積物內黏土礦物中伊利石含量最高，其次為綠泥石，高嶺石再次之，膨潤石含量最低。 在含量變化上，伊利石在南沖繩海槽由西向東遞減，結晶度表示其可能為近變質帶岩石所風化而來，主要來源為蘭陽地區所輸入之沈積物。綠泥石與高嶺石於棉花峽谷下緣及海槽中心有相對高值，且與濁流沈積有良好之正相關，顯示其為自陸棚或陸坡所傳輸而來。膨潤石的變化明顯看出與海槽中海底火山的位置有關。Esquevin-Index分析結果顯示海槽內沈積物中富鐵鎂伊利石與富鋁伊利石含量差異不大，幾處較低值可能與其源岩較多黑雲母類（Biotitic）岩石有關。 在南沖繩海槽沈積物樣本及東部各河川樣本中黏土礦物組成上，顯示海槽沈積物來源與陸上蘭陽地區輸出相關性較高，而花東地區河川沈積物供應量的比重可能較低。 本研究認為南沖繩海槽沈積物內綠泥石可能為富含鐵的鮞綠泥石（Chamosite），經由加熱處理方法時並無出現明顯綠泥石繞射峰值。 | zh_TW |
| dc.description.abstract | Clay minerals are one of the most useful indicators marine geology to decipher the source and transport of sediments in oceanography. The composition and distribution of clay minerals in sediments are related to the climate and the nature of their parent rocks.
In this study, the analysis result of the clay minerals illite is the most abundant clay mineral in the southern Okinawa Trough (SOT), the chlorite and kaolinite are more in the study area. The amount of smectite is the lowest in the sediment. The amount of illite increases from west to east SOT and the crystallinity of illite shows it might come from the weathering of rocks in the anchizone in the watershed of Lan-Yang River. The amount of chlorite and kaolinite is higher at the Mien-Hwa Canyon and the deepest part of SOT. The good correlation between chlorite, kaolinite and the turbidte distribution suggests that they were transported from the shelf or slope. We also observed that the amounts of smectite in the sediments are related to submarine volcanoes in the adjacent area. According to the Esquevin-Index, there is no difference between the amount of Fe,Mg-rich illite and Al-rich illite in the sediments of SOT. In some areas, the lower Esquevin-Index values indicate that the parent rocks might be more biotitic. Comparing the composition of clay minerals in the SOT and the riverine sediments of the Eastern Taiwan, we found that the Lan-Yang River is the most important source to the sediments in the SOT. | en |
| dc.description.provenance | Made available in DSpace on 2021-05-20T20:22:00Z (GMT). No. of bitstreams: 1 ntu-97-R94241302-1.pdf: 14174060 bytes, checksum: 600dd560a5e2856d458c3ca4a190f941 (MD5) Previous issue date: 2008 | en |
| dc.description.tableofcontents | 口試委員審定書……………………………………………I
致謝…………………………………………………………II 摘要…………………………………………………………III 目錄…………………………………………………………V 圖目錄………………………………………………………VII 表目錄………………………………………………………IX 第一章 緒論……………………………………………1 1.1、前言…………………………………………………1 1.2、研究區域……………………………………………1 1.3、前人研究……………………………………………5 1.4、研究目的……………………………………………7 第二章 研究方法………………………………………8 2.1、採樣區域………………………………………8 2.2、沈積物採樣……………………………………8 2.3、分析方法………………………………………12 2.3.1、樣本前處理……………………………12 2.3.2、X光繞射分析…………………………17 2.3.3、黏土礦物之定性與半定量分析………19 第三章 結果與討論……………………………………23 3.1、黏土礦物相對含量之分布……………………23 3.1.1、黏土礦物在空間面上的變化…………23 3.1.2、台灣東部河川樣本分析結果…………30 3.2、黏土礦物相對含量隨深度的變化……………32 3.3、南沖繩海槽表層沈積物中黏土礦物之來源討論……44 3.4、綠泥石測定的討論……………………………46 第四章 結論……………………………………………54 參考文獻……………………………………………………56 | |
| dc.language.iso | zh-TW | |
| dc.title | 南沖繩海槽表層沈積物中黏土礦物之研究 | zh_TW |
| dc.title | Clay Mineral Distribution in Surface Sediments of the Southern Okinawa Trough | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 97-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳汝勤,陳于高,魏國彥,洪崇勝 | |
| dc.subject.keyword | 南沖繩海槽,黏土礦物,X光繞射,鮞綠泥石, | zh_TW |
| dc.subject.keyword | clay minerals,southern Okinawa Trough,XRD,chamosite, | en |
| dc.relation.page | 124 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2009-01-31 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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