| 释义 |
Okinawa trough
基本例句
冲绳海槽
Wang, C., Yang, M.L., Chou, C.P. and Lee, C.S., 1998, Westward Extension of theOkinawa Troughin the Northern Taiwan Area: Morphology and Seismicity.王正松、周治平、李昭兴、杨敏郎，1998，台湾北部地区冲绳海槽向西之延伸。
Large amounts of microfossil records have been discovered in the seafloor black smoker chimney from theOkinawa Trough.报道了冲绳海槽伊平屋海洼海底黑烟囱样品中保留完好的矿化微生物群,它们的形态完好。
TheOkinawa Troughcan also be considered as an important link between East African Rift and Red Sea stage in the Wilson Cycle.冲绳海槽也可视为是威尔逊旋回中连接东非裂谷和红海阶段的一个重要的中间环节
The western end of the SouthernOkinawa Troughhas curvelinear bathymetric contours at the maximum depth of about 2,000m.宜兰海脊以东边的硫球岛弧为界，其区域范围有限，表现局部性的地形特徵。
TheOkinawa Troughis a marginal basin between the East China Sea shelf and the Ryukyu arc, with its axis running NE-SW.冲绳海槽内有三个基本的地貌单元;即西侧陆坡;槽底盆地和东侧岛坡.
The trapped particulates were mainly clay and silt in the north slope of Ilan ridge and south Okinawa trough, and were sand and silt in the Mien-Hwa canyon.宜兰海脊北坡与冲绳海槽的沉降颗粒，主要是黏土与粉砂，与棉花峡谷为砂及粉砂的 组成差异甚大。 |