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題名：臺灣花東海岸海階的地形學研究
書刊名：國立臺灣師範大學地理研究報告
作者：石再添
出版日期：1988
卷期：14
頁次：頁1-50
主題關鍵詞：地形學；花東；海岸；海階；臺灣
原始連結：連回原系統網址new window
相關次數：
  • 被引用次數被引用次數:期刊(6) 博士論文(3) 專書(0) 專書論文(0)
  • 排除自我引用排除自我引用:4
  • 共同引用共同引用:19
  • 點閱點閱:36
This paper is the first year report of the research project “A Geomorphological Study of Marine Terrace in Taiwan”. The Huatung coast is along the Pacific coast of Eastern Taiwan, adjacent to the convergent boundary of Eurasia Plate and Philippine Sea Plate, marine terrace is typically developed in this region. Based on air photo interpretation, geomorphometry, field excursion and accurate survey of altitude, the results are summarized as follows: 1. Classified and correlated by the continuity of altitude and extend of the marine terrace surfaces, there are three dominate marine terraces in study area. The flights of marine terraces in the southern part are comparatively more widely distributed than in the north, the lowest one and the newly raised wave-cut platform are well developed throughout the study area. 2. Altitude of terraces in the southern part is obviously more higher, expecially in the upper two steps, showing that there are wave-like uplifted and tilted slightly to the north. Yet the lowest steps together its newly raised wave-cut platform have almost the same height throughout the study area, this implies that recent uplift rates are progressing with equal amount, and in the upper steps, the tectonic movement has the property of accumulation. 3. The displacement of terrace surfaces is observed as a short-wave length warping, upwarping has been taken place with the axes in the vicinity of Chanping, Chengkung and Tulan, the distance between the axes is about 25 to 30 km. 4. The third steps are furnished with multi-levelled terraces, at intervals of 2-5 m in elevation, deduces from the mode of seismic uplifts in the neighborhood, those multi-levelled terraces may originated by the co-seismic uplift. 5. The features of marine terraces are also influenced by geological setting, in the area of more­resistant rocks, marine terraces are very narrow and covered with thin marine boulders, coastal landforms such as wave-cut benches, sea caves, notches are abundant. On the contrary, in the area of less-resistant rocks, terraces are more widely developed, and the bedrock often covered by thick layer of marine gravels and marine sand. 6. According to the altitude of terraces, using the method of correlation of global marine terraces that deviced by Bull, W.B. (1987), the uplift rate of central part of study area is 1.55m/Ka. The result indicate that the terraces are formed at the age of 64 Ka(I), 40 Ka (II) and 6 Ka (III).
期刊論文
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研究報告
1.劉平妹(1987)。台灣東部海階之新期變動地形研究（I，豐濱--成功段）。國立臺灣大學地質研究所。  延伸查詢new window
圖書
1.何春蓀(1982)。臺灣地體構造的演變。中華民國經濟部。  延伸查詢new window
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圖書論文
1.林朝棨(1957)。台灣地形。台灣通志稿卷一：土地誌．地理篇。台灣省文獻委員會。  延伸查詢new window
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5.Bloom, Arthur L.(1980)。Late Quaternary sea level change on south Pacific Coasts: A study in tectonic diversity。Earth Rheology, Isostasy and Eustasy。John Wiley and Sons。  new window
6.Bull, W. B.(1984)。Correlation of flights of global marine terraces。Tectonic Geomorphology。Boston：Allen and Unwin。  new window
7.Lajoie, K. R.、Kern, J. P.、Wehmiller, J. F.、Kennedy, G. L.、Mathieson, S. A.、Sarna-Wojcicki, A. M.、Yerkes, R. F.、McCrory, P. F.(1979)。Quaternary marine shorelines and crustal defor-mation, San Diego to Santa Barbara, California。Geological Excursions in the Southern California area。  new window
8.Ortlieb, Luc(1980)。Neotectonics from marine terraces along the Gulf of California。Earth Rheology, Isostasy and Eustasy。John Wiley and Sons。  new window
9.Ota, Yoko(1982)。Holocene marine terraces of uplifting areas in Japan。Holocene Sea Level Fluctuations, Magnitude and Causes。  new window
10.Schofield, J. C.(1980)。Postglacial tansgressive maxima and second-order transgression of the Pacific Ocean。Earth Rheology, Isostasy and Eustasy。John Wiley and Sons。  new window
11.Sutherland, D. G.(1983)。The dating of former shorelines。Shorelines and Isostasy。Academic Press。  new window
 
 
 
 
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