A Mode of the "URUMA" Crustal Movement in the Southeastern Part of the Okinawa-jima, Ryukyu Island

資料種別:
論文(リポジトリ)
責任表示:
Maruo, Yuji ; Furukawa, Hiroyasu ; Kizaki, Koshiro ; 丸尾, 祐治 ; 古川, 博恭 ; 木崎, 甲子郎
言語:
英語
出版情報:
琉球大学理工学部 — Science and Engineering Division, University of the Ryukyus, 1979-03
著者名:
Maruo, Yuji
Furukawa, Hiroyasu
Kizaki, Koshiro
丸尾, 祐治
古川, 博恭
木崎, 甲子郎
続きを見る
掲載情報:
琉球大学理工学部紀要. 理学編 = Bulletin of Science & Engineering Division, University of Ryukyus. Mathematics & natural sciences
通号:
27
開始ページ:
89
終了ページ:
98
バージョン:
publisher
概要:
The Ryukyu limestone of the Quarternary period develops well in the southeastern part of the Okinawa-jima, where it is regarded to be one of the type localities together with the underlying Shimajiri group. The limestone formation is divided into quite a few blocks by a series of faults representing platforms of various heights of 150 to 180m. The fault movement signifies the Uruma event of the Quarternary crustal movement. (Okinawa Quarternary Research Group, 1976, Kizaki and Takayasu, 1976). The present study based on the surface survey, drilling and electric prospecting shows that the structure of the limestone platform and the surrounding staircase topography of the area is resulted from a combination of uplift and subsequent concave landslide-like antithetic step faults. The period of the movement is defined here as after the sedimentation of the Ryukyu limestone and before the sedimentation of the terrace limestone which corresponds to the Machinato limestone of MacNeil (1960). 続きを見る
URL:
http://hdl.handle.net/20.500.12000/23767
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