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Owing to the continuous uplift since Quaternary, rejuvenated terraces, gorges and raised alluvial fans are developed well in the eastern slope of Coastal Range. The river terraces in this area are distributed below 200 m generally. The scarps of higher level terrace are larger than that of lower level one. The gravel deposits in higher level terrace are thicker than that of lower level one. Comparing the terrace between six studied rivers, meander terraces are significant both in Mawuku River, Fengpin River, Shuilien Riverand Fanshuliao River whereas fan terraces are developed well in Sanhsien River. In contrary, the terrace in Shuimuting River is undeveloped due to down cutting into hard rock which restricts the widening of terrace. By correlating to marine terraces, most of the terraces in this area are formed in Holocene. The detailed correlation of each step or dating still needs more envidences.

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潮州斷層帶的活斷層與地形

(國立台灣師範大學地理學系, 1983-10-??) 石再添; 鄧國雄

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琉球嶼的海階及珊瑚定年研究

(地理學系, 1991-03-??) 石再添; 張瑞津; 許民陽; 沈淑敏

The Liu-chiu Y? is a raised coral reef island, located southwest offshore 14 km from Tung-kang, Pintung Hsien. Two structural depression lines striking NE-SW and E-W separate the island into four blocks. The Liu-Chiu Y? Limestone overlays the Liu-Chiu Y? Mudstone with a uncon-formity relationship. Three steps of marine terraces can be recognized: Pleistonce I, Pleistonce II and Holocene terrace. Based on coral reef dating, elevation of samples and sea level curve, the average uplift rate of west coast is estimated about 2 mm/yr during the period from 34 ka to 10 ka YBP whereas 0.4 mm/yr in east coast since Holocene. The uplift and deformation of marine terraces are influenced both by the tectonic stress coming southweast and downwarping near Kao-Ping Drowned Valley.

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石門水庫集水域的河谷地形

(臺灣師範大學科學教育中心, 1978-09-??) 石再添; 鄧國雄; 張瑞津; 黃朝恩; 石慶得

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美、英、日三國主要地球科學課程的比較研究(上)

(臺灣師範大學科學教育中心, 1977-04-??) 石再添; 黃朝恩; 張瑞津