5)遠遠高於東海陸棚(<2),本研究中岩芯沉積物在0-12 ka的Chlorite / Kaolinite值(2-6)高於12-21 ka的Chlorite / Kaolinite值(0.5),推論12-21 ka東海陸棚為南沖繩海槽沉積物主要供應來源。 台灣沉積物與東海陸棚物質在主要元素K2O/TiO2比值上也有明顯差距,台灣沉積物的K2O/TiO2會高於東海陸棚的值,本研究中K2O/TiO2值(4.5)在12-21 ka遠遠低於0-12 ka及21-32.6 ka時的6-6.5,和黏土礦物變化趨勢一致,在12-21 ka時,東海陸棚物質輸入遠大於台灣東北部的貢獻。' > Airiti Library
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  1. 凌巧芸(2007) 南沖繩海槽地震引發濁流沈積物之來源及分布。國立台灣大學地質科學研究所碩士論文。
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  2. Aoki S., and K. Oinuma (1974) Clay mineral compositions in recent marine sediments around Nansei-Syoto Island south of Kyusyu, Japan, Journal of the Geological society of Japan, 80, 57-63.
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  3. Bernhard D., J. Hofmann, R. Herich, U. Rohl, and D. K. Futterer (unpublished) Detrital sediment supply at ODP site 1202 in the southern Okinawa Trough and its relation to sea-level changes, Kuroshio dynamics, and palaeoclimate during the last 30000 years , 23p.
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  4. Biscaye P. E. (1965) Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans, Geological Society of America Bulletin, 76, 803-832.
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  5. Chen C. T. A., R. Ruo, S. C. Pai, C. T. Liu, and G. T. F. Wong (1995) Exchange of water masses between the East China Sea and Kuroshio off northeastern Taiwan, Continental Shelf Research, 15, 19-39.
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