- 更多网络例句与等深线相关的网络例句 [注：此内容来源于网络，仅供参考]
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Comparing the changes of coast line, water depth contour line and deltaic flat slope in different period maps, we got the feature of deltaic flat changes.
对不同时期地形图的岸线、等深线、坡度变化的对比分析，得出不同岸段的变化特征。
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Shelf break at depths between 20 to 550 meters, with an average of 130 meters, also has the 200-meter isobath as the lower limit of the continental shelf.
陆架坡折处的水深在20～550米间，平均为130米，也有把200米等深线作为陆架下限的。
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The west of Qiandao port, that is near the Qiandao Village, the depth of water condition is good, the isobath of -5 meters is 3200 meters to the bank.
前岛港西部即前岛村附近水深条件较好，-5米等深线距岸3200米，开挖后可建设万吨级泊位。
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Advantage of the natural conditions:① Hankou port -6 m isobath offshore 1 km,-10 m isobath offshore 5 kilometers, the planned routes for various types of ships enter out, without tidal restrictions.
自然条件优势：①韩口港区-6米等深线离岸1公里，-10米等深线离岸5公里，规划的航道可供各类船只随进随出，不受潮水限制。
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Animal taxonomists described as a "living fossil" of the amphioxus, in the shallow water near the 15 m isobath density of 1035 / m, think about with these "living fossils" with swimming in a region, which can not but make you feel shock.
被动物分类学家誉为"活化石"的文昌鱼，在浅海15米等深线附近密度达到1035尾／平方米，想想能够与这些"活化石"同在一个区域游泳，这不能不使你感到震撼。
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It is shown from the analysis results that the average retrogradation rate of the south coastline of the Laizhou Bay during 1958 to 2004 was 27 m/a,the average retreating rate of the 0 m isobath was in the range of 27 to 65 m/a,and the average cutting rate of beach face was 2.1 cm/a.
结果表明，1958-1984年，莱州湾南岸岸线平均侵蚀后退速率为27 m/a，0 m等深线后退速率为27~65 m/a，岸滩平均蚀低速率为2.1 cm/a.1984-2004年，莱州湾南岸岸线位置基本无变化，岸滩平均蚀低速率为1.04 cm/a，水深5 m以浅的区域表层沉积物变粗。
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The shallow water and intertidal mudflat resources within isobath of 10 meters are about 368 thousand mu, with which 266 thousand mu of shallow sea area.
海域内10米等深线以内浅海与潮间带滩涂资源36.8万亩，其中浅海面积26.6万亩。
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There are a number of large and shallow beach Harbor, the 10-meter line, and other deep-shallow beach area of 74.3 hectares, the area available to 46.8 million, the 200 meters with isobath area of 53,000 square km of fishing grounds, suitable for aquaculture, coastal-rich sea salt.
有多处港湾和大片浅海滩涂，10米等深线内浅海滩涂面积74.3万亩，可利用面积46.8万亩，200米等深线内渔场面积5.3万平方公里，适宜海水养殖，滨海盛产海盐。
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Changes of erosion and accumulation of the seabed before and after the project The general characteristics of the pattern of erosion and accumulation of the seabed near the scheduled project both before and after the scheduled project are as the following: accumulation occurs at the areas lower than–10 isobath; some suspended sediment is deposited near the coast due to the relatively small tidal current with a monthly accumulation rate of 2-6 mm; while a slight erosion occurs in the areas deeper than–10 isobath with a monthly accumulation rate of .2 mm.
5工程前后海底冲淤变化工程前后海底冲淤相同的地方是：大致沿-10m等深线向近岸呈淤积状态，近岸由于潮流流速小，一些悬沙落淤，月淤积量在近岸附近约2-6mm；而-10m等深线以深基本上呈轻微冲刷状态，月冲刷量一般在0.2mm以下。
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The different points of views, transverse section, plane and volume changes are considered. The results show that the evolution of the Xinqiao Channel has experienced three stages: in 1861~1926 ,the Xinqiao Channel area had been eroded at first and then silted; the Xinqiao Channel is formed during 1926~1958 with the channel experiencing persistence erosion; from 1958 to 2002, the total volume of the Xinqiao Channel keeps stable with the volume of 5.02×108m^3. The pattern of 10m contour has shaped to a certainty in 1926 and 5m contour of the upper and lower parts of Biandansha has been joined. The change of sections of the Xinqiao Channel reflects its thalweg movement to the North Bank 1.1~2.8 km, its shape changes from "U" shape to "V" shape and its depth has been deepened.
计算结果显示在所研究的区域内自1861年以来新桥水道冲淤过程明显被分为三个阶段：1861~1926年的66a间新桥水道区域经过一段时间的冲刷后又重新产生淤积，总容积变化不大；1926~1958年的33a间新桥水道在不断的冲刷中总容积由2.603亿立方公尺增长到5.076亿立方公尺；1958年至今的45a时间里水道容积基本保持在平均5.02亿立方公尺。1926年新桥水道10m等深线已经形成一定的格局，1947年5m等深线向上延伸，扁担沙已经不再与崇明岛相连；1958年上下扁担沙的5m等深线基本连成一体，可以认为此时新桥水道已经形成。
- 更多网络解释与等深线相关的网络解释 [注：此内容来源于网络，仅供参考]
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fathom line：等深线
yearly expenditure 岁出 | fathom line 等深线 | sugariness 象砂糖, 甘味, 糖质
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isobath：等深线
isobarically 恒压的 | isobath 等深线 | isoceles triangle 等腰三角形
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isobath：等深线等深线
isobath 等深线 | isobath 等深线等深线 | isobathic chart 等深线图
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isobath：等深线;等高程线
isobasemap 等基线图 | isobath 等深线;等高程线 | isobathcurve 等深线
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isobath curve：等深线
isobase 等基线 | isobath curve 等深线 | isobath map 等深图
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water-table isobath：地下水位等深线
water-table gradient 地下水面坡度 | water-table isobath 地下水位等深线 | water-table outcrop 地下水露头处
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depth contours; isobath：等深线
深度基准面 depth datum | 等深线 depth contours; isobath | 等深距 isobath interval
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bathymetric chart：等深线海图;海洋水深图;世界大洋水深图
bathymetric chart 等深线海图 | bathymetric chart 等深线海图;海洋水深图;世界大洋水深图 | bathymetric contour 等深线
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isobathic line：等深线
isobathic chart 等深线图 | isobathic line 等深线 | isobathic 等深的
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isobathic chart：等深线图
isobath 等深线等深线 | isobathic chart 等深线图 | isobathic line 等深线