ocean basin 是什么意思

ocean basin的中文意思是: 海洋盆地

ocean basin例句大全

  1. The small ocean basin is formed and the ophiolite appear when back arc basin expands.

    弧后盆地扩张到达小洋盆,出现蛇绿混杂岩。

  2. From Late Devonian to Triassic, the period of paleo-Tethyan ocean ocean, the southwestern margin of Tarim

    晚泥盆世到三叠纪(古特提斯洋阶段),塔西南边缘经历了陆内裂谷/被动大陆边缘盆地-弧后伸展盆地-弧后前陆盆地发展旋回;

  3. Jurassic and Cretaceous, the marginal ocean basin was in the stage of ocean crust evolution and had a

    侏罗-白垩纪为洋盆洋壳演化期,处于类似洋中脊的构造环境。

  4. The flysch, with some basalts, is difference from modern ocean, but similar to arc-ophiolite sequence

    复理石沉积中夹较多的玄武岩,这与现代洋底不同,而与岛弧蛇绿岩层序有相似之处,代表早期初始洋盆型洋壳的残块;

  5. Study on the love wave / Rayleigh wave incompatibility in the Pacific Ocean Basin

    太平洋盆地勒夫波与瑞利波不一致性的研究

  6. Calcium carbonate dissolution belt and its character in the mid Pacific Ocean Basin

    中太平洋海盆碳酸钙溶解带及其特征

  7. A basin-wide ocean general circulation model is used to study the uptake and distribution of natural14C

    利用一个北太平洋海盆尺度环流模式模拟了北太平洋自然14C的分布和吸收。

  8. An ocean basin that persisted from the Paleozoic to Triassic did not exist, i.

    不存在从古生代延续到三叠纪的大洋盆地,即不存在所谓古特提斯或永久特提斯;

  9. A preliminary study on deep-sea carbonate dissolution cycles in Melanesia basin, Pacific Ocean

    太平洋美拉尼西亚海盆深海碳酸盐溶解旋回的初步研究

  10. Surface sediments and relationship between it and manganese nodules in Central Pacific Ocean Basin

    中太平洋海盆表层沉积物及其与锰结核的关系

  11. Preliminary results from a high-resolution Pacific-Indian basin-wide ocean general circulation model

    一个高分辨率太平洋-印度洋海盆环流模式的初步结果

  12. Petrologic restrictions on the Ordovician ocean basin scale and spreading rate in Qilian area

    北祁连奥陶纪洋脊扩张速率及古洋盆规模的岩石学约束

  13. The ocean basin became more narrow in early Late Paleozoic, which last several millions years.

    晚古生代早期的洋盆较狭窄,生存时间为数千万年。

  14. During subduction northward of Neo-Tethys oceanic plate, Ayla-Zhongba micro-continental, the marginal ocean

    在新特提斯洋板块向北俯冲消减过程中,阿依拉-仲巴微陆块、陆缘洋盆和印度大陆一起随着向北漂移,在印度大陆向北挤压作用下洋盆逐渐收缩以致最终闭合。

  15. Many volcanic eruptions along the ocean basin often go undetected because they can't be easily seen.

    许多沿海洋盆地的火山喷发往往不被发现,因为它们不容易被看到。

  16. Paleozoic siliceous rocks formed in the complex background of the coexistence of continental margin, ocean

    晚古生代硅质岩形成于大陆边缘、大洋盆地和洋脊共存的复杂背景下,指示这一时期的强烈构造拉张,在拉张强烈的部位形成了小洋盆和洋壳。

  17. A Discussion on the Problems About the Reconstruction of a Ancient Ocean Basin in a Continental Orogenic

    大陆造山带古洋盆恢复的有关问题讨论

  18. North Qilian region again stretched and suffered second oceanization, up to middle Ordovician a mature ocean

    早奥陶世北祁连地区再次拉张,遭受第二次大洋化,到中奥陶世形成具沟弧盆体系的成熟大洋。

  19. Major area of middle dangerous disaster of debris flows at Pacific Ocean Basin in northeast of China

    Ⅲ.东北太平洋流域危险泥石流区;

  20. There are large-scaled modern sediment waves wide-distributed on the deep-sea floors of the every ocean

    在世界各大洋深盆海底,均有大范围分布的现代大型沉积物波。

  21. The hanging wall siliceous rocks is deposited in a basin environment, with weak hydrothermal activity

    矿体顶板硅质岩沉积于热水活动明显减弱的环境,类似于大洋盆地构造环境下沉积的硅质岩;

  22. The structural environment forming the volcanic rocks was a rift ocean basin developed along the west

    火山岩形成的构造环境,是在扬子地块西缘基础上发展起来的裂谷洋盆,块状火山岩发育于裂谷洋盆中央(准洋脊),层状火山岩则发育于裂谷洋盆的陆缘斜坡(次大陆)。

  23. The Cretaceous-Tertiary Hehuai basin was generated owing to the combined effect of the Tethys and Pacific

    白垩-第三纪河淮盆地是在特提斯与太平洋动力学体系联合作用下形成的。

  24. Geochemistry of major and rare-earth elements of the basic volcanic rocks indicates the features of an ocean

    基性火山岩具大洋拉斑玄武岩特征,常量元素和稀土元素显示陆间洋盆性质。

  25. Many of our basin, a large basin with Sichuan Basin, Tarim and Junggar Basin and Qaidam Basin.

    我国盆地很多,其中大盆地有四川盆地、塔里木盆地、准噶尔盆地和柴达木盆地。

  26. On tye basis of the latter, it is devided into craton basin, fold basin, succeed basin, crack basin,

    依后者,可分为克拉通盆地、褶皱带盆地、继承性盆地、裂陷盆地、断陷盆地、陆缘盆地和侵蚀盆地等七种。

  27. In Early Palaeozoic stage the North Qilian ocean basin was a marginal sea environment induced from Paleo-Asiatic

    早古生代北祁连有限洋盆为古亚洲大洋诱发的边缘海环境,边缘海独特的的消亡历程形式形成了特征的成矿组合响应。

  28. It implys a MORB type ophiolite association and an ancient ocean basin between Qinling and Yangtze plates

    本区洋脊拉斑玄武岩为蛇绿岩的组成部分,指示一套MORB型蛇绿岩组合以及秦岭与杨子板块之间古生代中期&早中生代期间存在的一个古洋盆。

  29. provides important evidence for studying the ages of formation and elimination of the Central Asian ocean

    这一发现为研究中亚洋盆形成和消亡时代提供了重要依据,也为确定准噶尔盆地基底性质提供了重要线索。

  30. In the ocean basin spreading stage of Middle Silurian, it formed a increase metamorphic charateristics

    中志留世末洋盆扩张阶段,形成葡萄石、绿纤石相→低绿片岩相→角闪岩相的递增变质特征;

  31. collision orogeny in southern Tianshan occurred as the result of the closure of the northern Tianshan paleo ocean

    北天山古洋盆于晚石炭世的闭合导致了南天山碰撞造山作用。

  32. To evolution of west end of north Tianshan mountain in narrow ocean and formation of collision foreland

    其西北端和南部的发生与发展与北天山窄大洋西端的演化和碰撞前陆盆地形成有关;

  33. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be sub-ducted in

    以雅鲁藏布江带为主洋盆带的特提斯洋,从三叠纪晚期开始消减,经历了印支、燕山、喜马拉雅3个阶段脉动式板块汇聚造山过程。

  34. It is shown that the relative movement between the East Asian Continent and the Pacific Ocean Basin occurved

    反映了东亚大陆与太平洋盆相对运动的开始及东亚大陆真实边缘的产生。

  35. Indian Ocean and Southern Ocean Whale Sanctuaries

    印度洋和南极洋鲸鱼保护区

  36. The directions of the major tectonic stress fields for the basin are NNE-SSW and SN respectively during

    研究表明盆地区域主压应力场方向在加里东期呈NNE-SSW向和近SN向,主要是晚奥陶世以来秦岭洋盆向北俯冲并与华北板块碰撞的结果;

  37. This paper chiefly discusses sedimentary basin types, magmatism and basin formation, geodynamic setting

    本文着重讨论了沉积盆地的类型,岩浆活动与盆地形成,盆地形成的地球动力学背景,盆地形成、演化和改造与油气分布的关系等。

  38. The characteristics of aeromagnetic anomaly of continental slope and the oil and gas-bearing basin in

    中国东南地区及近海海域气溶胶反演遥感研究南海东沙以南海域陆坡航磁异常特征与含油气盆地

  39. The Neolithic culture Research in the Yalu river Basin, the Tumen River Basin and the Wusuli River Basin

    鸭绿江、图们江及乌苏里江流域的新石器文化研究

  40. The evolution of the basin can be divided into five stages, i. e.late Carboniferous rift basin, Permo-Triassic

    盆地演化可分为五个阶段,即晚石炭世裂谷盆地、二叠-三叠纪前陆盆地、侏罗纪伸展坳陷盆地,白垩纪-早第三纪破裂前陆盆地和晚第三纪-第四纪再生前陆盆地。