ocean floor

ocean floor的基本解释

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大洋底

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海底

与ocean floor相关的网络例句 [注：此内容来源于网络，仅供参考]

Use extensively at present be like next breed:(1) public go up with athletic car boat floor of ornamental flexibility balata ;(2) be able to bear or endure the balata floor that soda acid and chemical corrode;(3) floor of oil resistant balata ;(4) electric balata floor;(5) fight electrostatic balata floor;(6) floor of high report insulation;(7) high temperature resistant balata floor;(8) fight floor of ultralow temperature balata ;(9) floor of balata of Gao Naihou sex;(10) floor of tall resilience balata is waited a moment.

目前广泛使用的有如下品种：（1）公共场所和运动车船上作装饰用的弹性橡胶地板；（2）耐酸碱和化学品腐蚀的橡胶地板；（3）耐油橡胶地板；（4）导电橡胶地板；（5）抗静电橡胶地板；（6）高度电绝缘地板；（7）耐高温橡胶地板；（8）抗超低温橡胶地板；（9）高耐候性橡胶地板；（10）高回弹性橡胶地板等等。

Based on the data analysis and numerical simulation, the Arctic sea ice climate variability was researched, the result were as following:(1) The analysis on the seasonal cycle of the Arctic Ocean and atmosphere showed that: The seasonal surface wind is somewhat trade wind like in some regions in the Arctic. The surface air temperature is robustly determined from the underlying environments such as sea ice and Greenland glaciers. In the sea ice region the precipitation rate is larger than that of evaporation. Furthermore, the Arctic Ocean hydrology is profoundly influenced by the surrounding rivers discharge. These are the decisive factors on the ocean salinity pattern. Sea ice flux through the Fram Strait is larger in winter than in summer. From the 40s in the 20th century on, the ice volume flux has an increasing trend. The Arctic rivers flood season is about the melt period, the winter rivers discharge has a significant increasing. Correlation analysis shows that 7 to 10 years is a characteristic time scale that rivers discharge leads Fram Strait ice volume export.(2) Considering 9 major arctic rivers, the Arctic Ocean circulation was simulated through BOM. The result shows that: The BOM can reproduce the main Arctic Ocean circulation pattern. The"Islandization"which is commonly used in OGCMs to treat the North Pole, not only influences the ocean current near the pole, but also influences the current in the Northern Atlantic Ocean, thus the bogus island might influence global climate through thermohaline circulation in the Atlantic Ocean.

在资料分析和数值模拟的基础上，对北极海冰的气候变率进行了深入的研究，结果如下：(1)对北极地区大气和海洋季节循环特征的分析表明，气候平均风场在部分地区具有&信风&的性质；而气温场与海冰分布及格陵兰半岛冰原的下垫面特征有密切关系；在北极海冰区的降水量大于蒸发量，并且在全球大洋中北冰洋受到河流径流的影响最大，对北冰洋的盐度分布有决定作用；通过弗瑞姆海峡的海冰通量在冬半年大于夏半年，并且从20世纪40年代起，海冰的体积输送有增加趋势；北极河流的汛期主要在融化季节，冬季的河流流量有显著增加的趋势；相关分析表明7到10年是北极河流流量影响弗瑞姆海峡海冰体积输送的一个特征时间尺度；(2)采用BOM海洋模式对北冰洋海洋环流进行了模拟研究，在模式中考虑了北极9条主要河流的作用，结果表明该海洋模式可以较好模拟出北冰洋海洋环流的基本特征；多数大洋环流模式采用&北极岛化&的方法处理北极点，模拟结果表明&北极岛化&不仅影响到极点附近的海流，还会对相对较远的北大西洋海流造成影响，并可能通过大西洋的热盐环流对全球气候产生影响；(3)采用CSIM4海冰模式对北极海冰的气候态进行了模拟。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；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；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；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。

与ocean floor相关的网络解释 [注：此内容来源于网络，仅供参考]

ocean floor：海底

往昔对於深海床(deep sea-bed),海床(sea-bed),海底(Ocean floor)及底土(sea-soil)矿藏资源之开发,认为渺不可及. 近年深海床之无限蕴藏与技术可能性,使海底资源之开发,形成新的活动与新的争议. 一般而言,

ocean floor：海床

注二:大陆坡是介於大陆棚(Continental shelf)与海床(Ocean floor)之间的地段. 如图甲所示. 注四:大地槽(Geosycline)是一种盒形的地质构造,上面盖著厚厚的沉积物,如图乙所示. 图上还画出喜马拉雅山、昆仑山和西藏高原的成因.

ocean floor：洋底

ocean current 海流 | ocean floor 洋底 | ocean floor fracture zone 洋底断裂带

ocean floor：海底; 洋底

ocean environment 海洋环境 | ocean floor 海底; 洋底 | Ocean Heat Transport Experiment (OHTEX) 海洋热量输送实验

ocean floor spreading：海底扩张

ocean floor fracture zone 洋底断裂带 | ocean floor spreading 海底扩张 | ocean wave 大洋波浪