- 更多网络例句与地貌发生的相关的网络例句 [注：此内容来源于网络，仅供参考]
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Sediment from river is not the main source of the Rushan Bay now any more ,which leads to the change of balance of sedimentation power. Sediment will transport because of the drive of hydrodynamic elements in macroscopic view .Direction of suspended load is basicly the same as tidal current .Flood tide makes suspended load transport to tip of the inner Bay and to the Mouth in exterior Bay .The direction of longside sediment transport in two sides of the Mouth mainly focus in the Mouth .Because the coastline along the exterior Bay is very meandering and it belongs to the type of bedrock ,besides some sediment going into the inner Bay ,so actual net sediment discharge rate is less than calculation .It develops an ebb delta out of the Mouth and forms tidal sand ridge ,tidal washing canal ,barrier bar and marine physiognomy ;The result of model simulation disclosures that differences of sediment erosion and siltation between single tidal action and wave-current action are very big .From the analysis of sediment composition、sediment sources and stability of beach and ridge ,this article gets the conclusion that the channel has the possibility to silt ,though the course maybe very slow.
通过分析研究文章得出如下结论：沉积物平面分布与水动力的时空变化存在很好的相关性；口门外发育落潮流三角洲，形成潮流沙脊、潮流冲刷槽、浅滩、拦门沙等水下动力地貌；乳山湾河流来沙已不是湾内泥沙主要来源导致沉积水动力平衡发生改变，宏观上表现在泥沙受水动力驱动发生不断运移；悬沙运移方向与涨潮流方向基本一致，湾内涨潮流带来的悬移质泥沙向湾顶运移，湾外悬移质泥沙主要向口门方向运移；湾口两侧岸段沿岸输沙方向均指向口门方向，由于乳山湾外海岸线曲折，两侧岸段以基岩为主，加之部分泥沙进入湾内，实际净输沙量小于计算值；数值模拟发现潮流单独作用与波流共同作用下泥沙蚀淤模拟差别较大；从沉积物组成、泥沙来源及滩槽稳定性三个方面分析，文章认为研究区存在航道淤积的可能性，但过程相对较慢。
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Most environment pollutions appear mainly in karst region,especially in the form of water pollution; environment pollution has a much worse destruction to the earth,vegetation and physiognomy,especially in the quarry areas. It even results in geologic hazard; for the mine geologic hazard,the background of physiognomy is the potential factor,while the irrational exploitation is the magistral factor.
环境污染多出现在岩溶地区，以水污染为主；环境资源的破坏以露采区最为严重，对土地资源、植被、地貌景观有较大的影响，甚至对地质灾害的发生都有深刻影响；矿山地质灾害的发生，地质地貌背景是诱发的潜在因素，不合理的开采方法是诱发的主导因素，降雨和水文条件是激发灾难发生的直接原因。
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The graben geomorphic characteristics of Northern Xiqiangtang and Changjiang Riverhead depressions are obvious, whereas the Huanghe Riverhead and Ruoergai depressions are of relatively low development degree. However, they are products of the east-west geomorphic extensive deformation, and the dynamic background of the deformation is the same as that of the continental tectonic deformation of Qinghai-Tibet plateau.
其中西羌塘北部坳陷和长江源坳陷的地堑式裂陷地貌特徵明显，而黄河源坳陷和若尔盖坳陷发育程度较低，但它们均是在青藏高原大陆构造变形的统一动力学背景下，地貌发生东西向伸展变形的产物。
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The seasonally alternative distribution of wind and rainfall provides energy for soil erosion and loose underlying material, erodible soil types and landform also provide the material basis for desertification.
而河湖积和风积的松散土壤下覆物质和地形地貌及土壤特征都为荒漠化的发生和发展提供了物质基础。
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The results of rupture landform investigation indicate that this fault is one of weak active faults in Holocene, its average vertical slip rate is 0.5~0.6mm/a. On Jun. 15, 1975, Liuba M6.2 earthquake in Kangding occurred on the fault. The macro-epicenter located at Shuobu-Moda, Liuba county. The direction of long axis of meizoseismal area is same as that of Yunongxi fault trend. The occurrence of the earthquake is resulted from the newest activity of the fault.
断错地貌研究结果表明，该断裂为一条全新世弱活动断裂，平均垂直滑动速率为0.5~0.6mm/a左右。1975年1月15日康定六巴6.2级地震发生於该断裂上，宏观震中位置位於六巴乡溯布－莫达村附近，极震区长轴方向与玉农希断裂走向一致，是该断裂最新活动的表现。
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The long axis of the high intensity isoseism of this earthquake is NE-trending, consistent with the Haiziyan Fault, which is therefore assumed to be the seismogenic fault of this earthquake.
五原6.0级地震高烈度区等震线长轴呈NE向，与海子堰断裂一致，是五原地震的发震构造。1996年包头西6.4级地震发生在由陡崖和沟槽地貌显示的NEE向乌拉山北缘断裂与NW向新生砂石厂断裂交会的部位。
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When the shockwave energy weakened, mountain collapse often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase slope slide (primary meteorite-stricken slope slide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; during the long geological ages after the formation of meteorite crater, under the action of erosive transit and dryness and humidity of hydrosphere and air current, volcano and earthquake activities, etc., the physiognomy gradually reverts to the original state.
在冲击波能量减弱时，环形山原来较陡峭的内侧多发生山体崩塌，外侧山体发生斜岩滑坡，在余震中山体构造不断调整以达到重力平衡；在漫长的地质年代里，陨击坑成型以后，在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。
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When the shockwave weakened, landslides often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase avalanche (primary meteorite strike landslide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; after the formation of meteorite crater, during the long geological ages, under the action of hydrosphere, erosive transit and dryness and humidity of air current, volcano and earthquake activities, etc., the landform gradually reverts and returns to the original state.
在冲击波能量减弱时，环形山原来较陡峭的内侧多发生山体崩塌，外侧山体发生斜岩滑坡，在余震中山体构造不断调整以达到重力平衡；在漫长的地质年代里，陨击坑成型以后，在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。
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The research shows clearly that the application of coastal multisource geospatial platform has changed the traditional coastal geomorphological science dramatically from its research scope, fields and methods, however, as made clear, extracting accurate information from remotely sensed data and GIS databases for coastal geomorphological applications is a nontrivial challenge that requires the combined knowledge and skills of information scientists and geomorphologists.
通过上述方法体系与应用研究说明，以GIS为核心建立的多源地理空间信息平台使传统海岸海洋地貌研究的范围、内容及方法都发生了重大变化，但多源数据信息的精确解译和成功应用必须同时具有空间信息学和地貌学专家知识。
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On the basis of previous research and the authors' field investigations,it is thought that the complex geological structures,strong crust movements and rivers erosions,frequent earthquakes,abundant loose deposits,favorable geomorphology,well-developed modern glaciers and plentiful precipitation are the principal causes of triggering frequent mudflows in the study area.
根据前人的成果以及作者的实地调查，认为复杂的地质构造、强烈的地壳运动和河流切割、频繁的地震、丰富的松散堆积物、有利的地形地貌、现代冰川以及丰沛的降雨是研究区泥石流灾害频繁发生的主要原因。
- 更多网络解释与地貌发生的相关的网络解释 [注：此内容来源于网络，仅供参考]
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morphogenetic：地貌成因的
morphogenesis 地貌成因 | morphogenetic 地貌成因的 | morphogenic phase 地貌发生幕
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morphogenetic：形态发生的 形态形成的 地貌成因的 地貌发生的
morphogenesis 地貌成因 地貌发生 形态发生 | morphogenetic 形态发生的 形态形成的 地貌成因的 地貌发生的 | morphogeneticforce 地貌发生力
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uniformitarianism：地质均变论
书中阐述的地质均变论(uniformitarianism)提到,历史上地质的侵蚀、沉降过程,以及火山活动发生的频率和现在是一致的. 莱尔还否定了当时流行的地质灾变说(catastrophism),他认为地貌并不由超自然能量引起的突发剧烈地质活动决定.
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morphogenic：地貌成因的
morphogenic phase 地貌发生幕 | morphogenic 地貌成因的 | morphogeny 地貌形成作用
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morphogenic phase：地貌发生幕
morphogenetic 地貌成因的 | morphogenic phase 地貌发生幕 | morphogenic 地貌成因的