Researchers have discovered a potential new species of comb, or ctenophore, jellyfish near the Ryukyu Trench near Japan.
在日本附近的琉球海沟，研究者们发现了栉水母的一个可能新种。
From then on, Ryukyu Buddhism didn't exist any more.
从此，琉球佛教之名亦不复存在。
Okinawa ocean trough and Ryukyu island arc were formed in late Miocene.
中新世晚期，冲绳海槽和疏球岛弧形成。
Fuzhou Ryukyu Hotel played an important role in the association between China and Ryukyu.
福州琉球馆在当时的中琉交往中发挥着重要的历史作用。
The Ryukyu current is a northeastward and western boundary current east of Ryukyu Islands.
琉球海流是琉球群岛以东一支东北向的西边界流。
An island group of the central Ryukyu Islands in the western Pacific Ocean southwest of Japan.
位于西太平洋，日本西南部的琉球群岛中部的一个岛屿群。
An arm of the western Pacific Ocean bounded by China, South Korea, and the Ryukyu and Kyushu islands. It has rich fishing grounds.
西太平洋的一片海域，沿岸为中国、韩国、琉球群岛和九州岛所包围，此区鱼资源丰富。
The east slope is slow, and is the inserting side from the northwest Philippine Plate into the Ryukyu Island Arc, connecting with the ocean basin.
东坡（洋坡）缓，是西北菲律宾海板块向琉球岛弧下插的一边，与大洋盆地相连。
This article will prove that how Ryukyu Annals written by Zhouhuang forms into a book and its edition, generalize the contents, and discuss its documentary value.
本文考论了清周煌所撰《琉球国志略》的成书情况及其版本，简括了其内容，论述了《琉球国志略》的文献价值。
The results show that Kuroshio intrudes onto the continental shelf of East China sea in large scale and during its flow water is exchanged ceaselessly with outer sea along Ryukyu Island.
模拟结果表明黑潮在东海陆架有大规模的入侵，其在沿东海陆坡流动途中沿着冲绳岛与外海不断的进行水体交换。
In the regions east and south of the Ryukyu Islands, there are some mesoscale cyclonic and anticyclonic eddies with different scales, and the variability of their character is also reviewed.
最后指出在琉球群岛以东、以南海域，经常出现各种不同的中尺度反气旋式和气旋式涡，讨论了它们在时间与空间尺度上变化的特征。
The Northern Min culture centered on Fuzhou is marked by the early adoption of Buddhism, and shows influences of Japanese culture and Japanese cuisine through contacts made with the Ryukyu Islands.
闽北文化以福州地区为中心，它的典型特征是佛教特色比较浓重，同时在历史上由于与琉球群岛往来频繁，因而又深受日本文化及饮食的影响。
These characteristics reflect that couplings between the upper arc and the subduction slab of the Ryukyu trench are weak relative to other common trenches, and themselves weaken toward to the south.
这些特点说明琉球沟弧系上覆板块与俯冲板块的耦合比其他沟弧系弱，而琉球海沟本身又往南趋弱。
These characteristics reflect that couplings between the upper arc and the subduction slab of the Ryukyu trench are weak relative to other common trenches, and themselves weaken toward to the south.
这些特点说明琉球沟弧系上覆板块与俯冲板块的耦合比其他沟弧系弱，而琉球海沟本身又往南趋弱。
应用推荐