- 更多网络例句与向陆的相关的网络例句 [注：此内容来源于网络，仅供参考]
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When forecasting wind speed to wind farm at coast, if there is land sea breeze, we can use the characteristic of wind profile using stastical method to correct the forecasing by model.
并发现即使没有海陆风发生，当风向为海洋吹向陆地时，风速随高度的垂直切变同样小于陆地吹向海洋的时段。
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It is an intracontinental deformation system resulting from the structural stress caused by the collisions of the Huaiyu terrane moving westwards and the Cathaysia block moving northwestwards.
江南古陆与华夏古陆拼接带北西侧前震旦纪地层中存在着近东西向褶皱叠加在早期近南北向褶皱上的现象，这是怀玉地块向西拼贴、华夏古陆向北西碰撞拼接过程中构造应力向陆内传递时形成的构造变形系统。
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Pulling setting presents in southern China in Permian forming rift basins, which extends and develops from the edge to the inside of continent. Under the influence of Dongwu movement, two second order cycles forming by up and down of sea level happened in Yangtze and Huaxia craton. Rift basins in continental margin are primary sedimentary location of LST. But craton areas are the main deposition area of TST and HST. Weathering on land and river sediment or only thin coaly clasolite of marsh facies present mainly in LST deposition.
二叠纪我国南方总体处于拉张背景，发育了由陆缘向陆内延伸发展的裂陷盆地；受东吴运动影响，扬子和华夏克拉通遭形成了两个二级海平面升降沉积旋回；陆缘裂陷盆地是低位期沉积的主要场所，而克拉通区主要为海侵和高位期沉积，低位期主要表现为陆上风化残积、河流沉积或仅发育厚度很薄的沼泽相含煤碎屑岩。
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The tectonic effect by foreland basin system might not be significant since Kueichulin Formation corresponded to eustatic sea level change and the Kueichulin Formation might means an unaffected tecton - sediemntary unit. The locality might be the hinge of forebulge flex.
前凸起的运动模式应为以垂直向上抬升为主，而非有向陆迁移之现象之外，而其发生时间应为6.5 - 5.6Ma；由於桂竹林层仍符合全球海水面变化，则其表示了一个在前陆盆地系统挠曲行为中一个较不被影响的构造单元，则此应为前凸起之枢纽带位置。
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Phragmites Australis, Ael uropus liitoralis, Zoysiamacrostachya, Messerschmidia sibirica, Limonium bicolor were the main vegetation types in the chenier seaside, but in the chenier plain, Artemisia annua, Artemisia mongolica and Herba Heteropappi Altaici occurred frenquently.
通过对无棣贝沙堤植物多样性的分析发现，样方内共出现物种20余种；同时，贝沙堤向海面和贝壳滩脊、向陆一面分别分布着以芦苇、獐茅、大穗结缕草、二色补血草、砂引草以及以青蒿、蒙古蒿、阿尔泰紫菀为优势种的群落。
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The rocks were probably situated in the followup obduction of split upper crust cover of the Yangtze Plate onto the North China Plate in or after the subduction of the Yangtze Plates continental materials towards the North China Plate,or were placed by southward thrusting when ultrahighpressure metamorphic rocks underpinned.
通过露头的构造地质分析，推断本套地层是在扬子板块陆壳物质向华北板块下深俯冲过程期间或其后扬子板块陆壳上部盖层继续向华北板块仰冲就位的，在超高压变质岩折返时经历了由北向南的逆冲。
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Exhibiting angle unconformities or erosion unconformities in different part of the basin, these surfaces are obvious to be recognized on seismic profiles.T1 conformity, separating Eogene from Neogene, was formed during the whole basin uplifting and erosion by the end of Eogene.T1 unconformity denuded unbearing strata differently, and the deeper and thickest erosion lies on the southern margin of the basin, which reflects the activity of southern Jiangnan paleo-terrene. In conclusion, the major erosion belts extending along NW direction reflects NE-SW compression and slipping caused the Eogene basin uplift and strengthen the earlier NW direction extending low convex, and formed the NW direction extending depress and erosion belts.
古近系和新近系之间的T1不整合面形成于古近纪末期的盆地整体抬升，对下伏地层造成不同程度的剥蚀，沿盆地南缘的剥蚀层位深，剥蚀量大，反映盆地南缘整体相对隆起，与江南古陆的隆起作用有关。T1界面剥蚀带走向以北西向为主，反映了盆地在古近纪末受到了北东－南西向的挤压或压扭作用，该作用造成盆地整体抬升，强化了北西向展布的低凸起，产生了近北西向的洼陷和剥蚀带。
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During the period of the astronomical evolution the Gondwana land formed at the south pole and high latitude areas. At the early stage of geological evolution the horizontal motion of magma might have driven the original crust to split and its northern edge might have drifted to where the outer-core liquid converged i.
在天文演化阶段，冈瓦纳古陆形成于南极；在地质演化阶段，南半球表层液核流体获得向东北的速度，同时导致了冈瓦纳古陆的分裂和漂移。
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In the Paleozoic era,the northern border area of North China Craton belonged to the tectonic domain of south peri-Paleozoic ocean and is characterized by subduction-collision orogenesis,leading to the formation of EW- to ENE-trending folds,thrust faults,nappes and ductile shear zones etc.
古生代，华北地块北缘处于古亚洲洋构造域，造山作用属陆缘俯冲-碰撞型，形成以EW向至NEE向为主的褶皱、逆冲推覆构造及韧性剪切带等构造类型。
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The bank capitalises on its onshore presence across Asia, Africa and the Middle East to offer customers convenient and reliable access to the widest range of currency markets, to date local market information, country-specific global risk management strategies, and customised capital raising and liquidity management solutions.
提供客户方便的和可靠的接触最宽范围的通货横过亚洲，非洲和中东的在它向陆的出现上的银行 capitalises 在市场上销售，约会地方市场数据，国家-特定的全球危险管理策略，而且订制了首都升起和流动性管理解决。
- 更多网络解释与向陆的相关的网络解释 [注：此内容来源于网络，仅供参考]
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brackish water：微咸水
我国不少文献[16~19]习惯把盐度仅在1~10的微咸水(brackish water)即视为"盐水",这种微咸水的随潮向陆上溯运动便认为是"盐水入侵",其垂向盐度等值线向陆倾斜分布的现象每被当成"盐水楔".
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inshore：近海的
inshore 近海岸的 近岸的 向陆的 | inshore 近海的 | inshorebreeze 海风
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inshore：近海岸的;近岸的;向陆的
inset 插入物 | inshore 近海岸的 近岸的 向陆的 | inshore 近海的
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landward：向陆的
landtied 陆连的 | landward 向陆的 | landwards 向陆地
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landward：近陆的
landward 向陆的 | landward 近陆的 | landwards 向陆地
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landward：向陆的/近陆的
landsturm /国家总动员/ | landward /向陆的/近陆的/ | landwards /向陆地/
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SIB：西伯利亚
网站描述: 在前寒武纪最晚期和古生代早期,超级大陆Rodinia位于南极附近,其后,发生开裂,各个块体纷纷向北飘移. 这些陆快中最显著的包括北美洲陆快(Laurentia),Baltica和西伯利亚(SIB)陆块.
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anadromous salmon：沿河产卵的大麻哈鱼
anadromous migration | 溯河回游(向陆回游) | anadromous salmon | 沿河产卵的大麻哈鱼 | anadromous | (海鱼)溯河产卵的
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Vines：藤
就可向灯塔前进.与灯塔管理者交谈得知向南的路不可能通过,(陆的不行找水的)灯塔后面用小刀取 得藤(vines),再用藤将木板(boards)绑在一起造木筏(raft)就可向West Shanbar出发.桥下男孩(Waif)不要吓他,
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salt water：盐水
但其中的"盐水"(salt water)何所指,淡水究竟是在和谁(什麽水)发生混合,不同的人有不同的理解. 我国不少文献[16~19]习惯把盐度仅在1~10的微咸水(brackish water)即视为"盐水",这种微咸水的随潮向陆上溯运动便认为是"盐水入侵",