臺灣學術機構典藏系統 (Taiwan Academic Institutional Repository, TAIR)

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Institution	Date	Title	Author
國立臺灣海洋大學	2010-11-15	A multiproxy lake record from Inner Mongolia displays a late Holocene teleconnection between Central Asian and North Atlantic climates	Huei-Fen Chen;Sheng-Rong Song;Teh-Quei Lee;Ludvig Löwemark;Zhenqing Chi;Yong Wang;Eason Hong
國立臺灣海洋大學	2010-01	Geomorphic Evolution of a Barrier Island Reflects the History of Natural Sediment Supply and Human Intervention in Taiwan	Eason Hong;W. Brian Dade;Yet-Chung Chang;Shun-Yu Chan
國立臺灣海洋大學	2007-09	The Influence of the Beach Environment on the Digging Success and Nest Site Distribution of the Green Turtle, Chelonia mydas, on Wan-an Island, Penghu Archipelago, Taiwan	Ho-Chang Chen;I-Jiunn Cheng;Eason Hong
國立臺灣海洋大學	2006-10-01	Shifting submarine canyons and development of a foreland basin in SW Taiwan: controls of foreland sedimentation and longitudinal sediment transport	Ho-Shing Yu;Eason Hong
國立臺灣海洋大學	2004-11	Morphology and Dynamic Sedimentology in front of the Retreating Tsengwen Delta, Southwestern Taiwan	Eason Hong;Tien-Chi Huang;Ho-Shing Yu
國立臺灣海洋大學	2000-05	The Future Impact Of The Tanshui Harbor On Its Nearby Coastal Environment	Eason Hong;Chung-Hung Ou;Shin-Sheng Tseng;Nan-Jong Kuo;Ten-Chi Huang;Wen-Chi Lee
國立臺灣海洋大學	2000-03	Echo characters and sedimentary processes along a rifting continental margin, northeast of Taiwan	Eason Hong;I Shih Chen
國立臺灣海洋大學	1999-11	Mechanisms Influencing the Spatial Distribution of Trace Metals in Surficial Sediments off the South-Western Taiwan	Tien-Hsi Fang;Eason Hong
國立臺灣海洋大學	1997-08	Evolution of Pliocene to Pleistocene sedimentary environments in an arc-continent collision zone: Evidence from the analyses of lithofacies and ichnofacies in the southwestern foothills of Taiwan	Eason Hong
國立臺灣海洋大學	1996-03	A Study on the Bathymetry and Sediment Distribution off Tanshui Estuary	Eason Hong;Jiang-Shiou Hwang;Cheng-Han Tsai;Chin-Houng Ou
國立臺灣海洋大學	1995	淡水河口外海一帶初步之海洋地質研究	洪奕星;蔡政翰;黃將修;歐俊宏; Eason Hong;Cheng-han Tsai;Jiang-shiou Hwang;Chung-hung Ou

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