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冲绳海槽是一个构造上极其活跃的大陆坡边缘盆地,具有壮观的海底地貌形态。研究冲绳海槽地区构造作用与其地貌演化的关系,有助于我们进一步深入了解冲绳海槽本身的地质演变历史,其意义非常重要。本文系根据1980年以来对冲绳海槽多次地质、地球物理调查所获得的一系列成果,结合前人已有的一些资料撰写而成。笔者拟将对冲绳海槽地区路作用与地貌演化的关系作一初步探讨,不足之处,恭请惠正。
The Okinawa Trough is an extremely active continental margin basin with a spectacular seabed topography. Studying the relationship between the tectonic role of the Okinawa Trough and its evolution can help us to further understand the history of the geological evolution of the Okinawa Trough, and its significance is very important. This article is based on a series of achievements obtained from the multiple geology and geophysical surveys of the Okinawa Trough since 1980, and based on some existing data of our predecessors. I intend to conduct a preliminary discussion of the relationship between the role of the Okinawa Trough area and the evolution of the terrain, inadequacies, Christopher Hui right.