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目前,有关琉球弧的陆域资料掌握的甚少。要详细研究琉球弧的形成史,需充分考虑近海海底地质,并掌握近海陆域地质资料。为了探讨琉球弧的形成史,笔者曾分别在1980和1983年就陆域、海域两者间的相互关系提出了一些假设,其中部分假设正在被证实,另外,又提出了一些新假设。本文介绍的仅是其中的一部分。正如笔者(1985c)所叙述的那样,[地球]杂志1985年12期的专题为小笠
At present, there is little information on the land-based information about the Ryukyu Arc. In order to study the formation history of the Ryukyu Arc in detail, it is necessary to fully consider the offshore seabed geology and grasp the geological data of offshore land areas. In order to explore the formation history of the Ryukyu Arc, I made some assumptions about the interrelationship between the land area and the sea area in 1980 and 1983, respectively, some of which are being confirmed. In addition, some new hypotheses are put forward. This article describes only some of them. As the author (1985c) states, the theme of [Earth] magazine in 1985 is Xiaoli