1) the central Okinawa Trough
冲绳海槽中部
1.
Core Z14-6(27°07′N,127°27′E,and water depth 739 m) retrieved from the central Okinawa Trough was selected for planktonic foraminifera and calcareous nannofossil study.
对取自冲绳海槽中部的Z14-6岩心进行了钙质超微化石的鉴定统计和有孔虫的氧碳稳定同位素分析,在利用浮游有孔虫氧同位素曲线对比进行地层划分的基础上,通过与邻近区域3个岩心数据进行对比,分析了150kaBP以来该海区钙质超微化石下透光带属种Florisphaera profunda百分含量变化特征及其受控机制。
2) the middle and southern Okinawa Trough
中、南部冲绳海槽
3) Southern Okinawa Trough
冲绳海槽南部
1.
Preliminary Study on the Radiolaria from the Surface Sediments in Southern Okinawa Trough;
冲绳海槽南部表层沉积物中放射虫的初步研究
2.
Benthic foraminiferal distribution in surface sediment along the con- tinental slope of the southern Okinawa Trough : dependance on water masses and food supply;
冲绳海槽南部表层沉积中底栖有孔虫分布:水团和食物供应的共同制约
4) Northern Okinawa Trough
冲绳海槽北部
1.
The rock magnetic behavior og gravity core CSH1 from the northern Okinawa Trough and the effect of early diagenesis;
冲绳海槽北部CSH1孔岩石磁学特征及其早期成岩作用的影响
2.
Through the analysis of 84 samples collected from the core B-3GC in the northern Okinawa Trough, a high resolution dinoflagellate cyst record of the Holocene has been obtained.
通过B-3GC柱状样84个样品的分析,获得了冲绳海槽北部全新世高分辨率沟鞭藻孢囊记录。
3.
Planktonic foraminifera, oxygen and carbon isotopes have been studied in core DOC-42 from the continental slope of the northern Okinawa Trough to reconstruct the paleoenvironmental evolution history of the surface water.
利用AMS 14C年代测试、氧同位素分析和浮游有孔虫分析重建了冲绳海槽北部陆坡 DOC 42 孔约 44cal。
6) Okinawa Trough
冲绳海槽
1.
Computation of Thickness of Hydrate Stability Zone in Okinawa Trough;
冲绳海槽天然气水合物稳定带厚度的计算
2.
Development and distribution of natural gas hydrate in the Okinawa trough;
冲绳海槽天然气水合物的发育与分布
3.
The physico-chemical features and their geological implications of magma in the Okinawa Trough;
冲绳海槽岩浆物理化学性质及其地质意义
补充资料：冲绳海中公园
冲绳海中公园
冲绳海中公园坐落于海中的望塔上，可以看到翡翠般的海水、千姿百态的珊瑚礁、五彩缤纷的热带鱼。冲绳美丽而广阔的海域是世界海洋生物的巨大宝库之一。澳大利亚的大堡礁是世界最大的珊瑚群，但冲绳的珊瑚种类并不比大堡礁逊色多少，冲绳的珊瑚种类多达68属260种，堪称世界第一。公园附近的细长沙滩、海水浴场、海洋体育娱乐项目，也令游客乐趣无穷.
说明：补充资料仅用于学习参考，请勿用于其它任何用途。