Okinawa Trough中文,Okinawa Trough的意思,Okinawa Trough翻译及用法

2026-03-21 23:23 浏览次数 27

Okinawa Trough

The (also called , literally China-Ryukyu Border Trough ) is a seabed feature of the East China Sea. It is an active, initial back-arc rifting basin which has formed behind the Ryukyu arc-trench system in the West Pacific.

Okinawa Trough 例句

英汉例句

  • The oxygen isotype method was used to test the hydrothermal chimney and sulfide samples collected from the Mariana Island Arc, the Mariana Trough, the Okinawa Trough and the Galapagos Rift.

    使用氧同位素方法 ,测试了西太平洋马里亚纳岛弧、马里亚纳海槽、沖绳海槽和东太平洋加拉帕戈斯裂谷的海底热液烟囱和硫化物全巖样品。

  • The Okinawa Trough (OT) is the solitary active backarc basin in the world that is formed by extensional rifting in the continental marginal zone and is in the early stage of evolution.

    沖绳海槽是当今世界上唯一的在大陆边缘张裂形成的、处于早期演化阶段的活动性大陆边缘弧后盆地。

  • According to the tectonic stability and heat flow, the north part and south part of the Okinawa Trough are the most perspective area for the gas hydrate explorations.

    根据热流、构造活动性和稳定带的厚度分析,研究区北部和南部更适合天然气水合物的稳定赋存。

  • The sedimentation rate (SR) of the middle Okinawa Trough of the last glacial period is mainly controlled by the sea level change and the wetness of the source area.

    末次冰期以来沖绳海槽中部沉积速率的变化主要受海面变化和物源区气候湿润程度的控制。

  • It is considered that the crust in the Okinawa Trough area belongs to the transition type, which is quite similar to the feature of the oceanic crust.

    综合分析认为:沖绳海槽地壳属于过度型地壳,与大洋地壳的许多特点颇为相似。

  • The submarine hydrothermal mounds in the Middle Okinawa Trough may be the shsllowest ones in the world.

    沖绳海槽中部南奄西海丘海底热液活动为弧后盆地型热液活动。

  • This paper illustrates good prospective to seek gas hydrate in the Continental Slope and Okinawa Trough in the East China sea, according to the research of 2d seismic profiles surveyed by our bureau.

    本文根据我局在沖绳海槽区的二维地震剖面研究,发现东海陆坡—沖绳海槽区具有天然气水合物的较好远景。

  • According of east abyssal plain of the Okinawa Trough with some volcanic materials, it show strong magnetic characteristics different from other sediment environments.

    沖绳海槽东槽底平原沉积物含有较多的火山物质,磁学特征与其它沉积环境有明显差异,各磁性参数特征值也明显较强。

  • The basement tectonics in the north of Okinawa Trough was deduced using the latest gravity and magnetic data.

    利用最新的重磁数据对沖绳海槽北部的基底构造进行了推断解释。

  • It is shown from the analysis results of grain size data that the sediments from the northern Okinawa Trough are mixture of terrigenous materials and volcanic ash during the Holocene epoch.

    沉积物粒度数据的端员分析结果表明,沖绳海槽北部全新世沉积物中的硅酸盐碎屑是由陆源碎屑物质和火山灰按不同的比例混合而成的。

  • The research result on element isotopes shows that the characteristic of the crust in the Okinawa Trough area is different from that in East China area and the Ryukyu Island Arc area.

    元素—同位素研究表明:它不同于中国东部,与琉球岛弧地区的特点也不相同。

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