堆积地貌

  • 网络accumulation landform
堆积地貌堆积地貌
  1. 针对洞里萨湖地区特殊的堆积地貌环境,采用先对SRTMDEM数据进行负值转换再提取水系的方法,取得了很好的效果。

    Aiming at Sap Lake area for the accumulation of special landscape environment , the first use of anti-SRTM DEM data to extract water from the method and achieved very good results .

  2. 沟道粘性泥石流堆积地貌的成因分类

    Genetic classification of accumulational landforms of channel viscous debris folw

  3. 这两个阶段在水体外貌与泉华堆积地貌上均有明显的表现。

    These two phases perform absolutely in water exterior and sinter sedimentary physiognomy .

  4. 沉积物的粒度结构受堆积地貌及水动力的大小、状态而制约。

    The grain structures of sediments were limited by the sizes and shapes of accumulation form and river flow .

  5. 本文分析了滑坡的成因和滑动的机制,根据滑坡运动后的残留痕迹和堆积地貌特征,认为头寨沟滑坡的运动方式和路径独具特点。

    Based on the traces of remains and depositional landforms of landslide , the auther thinks that the landslide movement has its special pattern and track .

  6. 浙江花岗岩地貌可分为花岗岩峰丛、花岗岩山丘、花岗岩石蛋和花岗岩崩塌堆积地貌等。

    The Zhejiang granite landforms may be classified into the granitic peak cluster , granitic hill , granitic rock and collapse pile landforms and so on .

  7. 前人的研究发现风蚀坑多发展为风沙堆积地貌,例如抛物线型沙丘或线性沙丘,而本区风蚀坑则可发展为其他类型的风蚀地貌。

    Previous study found that blowouts will evolve into wind-accumulated landform , such as parabolic dunes or linear dunes . However , blowout in this area can evolve into other types of wind eroded landforms .

  8. 配套的剥蚀地貌、侵蚀地貌和堆积地貌;如遇洪水年,当洪峰流量超过60000m3s时,中、下游河道水位明显抬高而进入防汛警戒状态,河床有明显冲淤变化;

    When the flood peak water discharge exceeds 6,000 m 3 / s at the Datong Station , the water level of the middle and lower reaches of the river arrives at the flood preparation cautionary state and the riverbed changes obviously due to erosion and accumulation ;

  9. 泥石流堆积扇地貌特征及其模型试验研究

    The geomorphological characteristics of debris fans and their model experiments

  10. 物质的侵蚀-搬运-堆积是地貌发育的主要过程。

    The erosion-transport-deposit of weathering sediment is one of the important process of geomorphology development .

  11. 浙北嘉湖全新世堆积平原地貌发育过程与土壤形成的关系

    The Relations Between the Development Course of Landform and Soil Formation in Jiaxing-Huzhou Holocene Sedimentary Plain of North Zhijiang

  12. 从古堆积体地形地貌特征、粒度特征以及形成时的古气候环境三方面对其成因进行分析。

    This paper will analyse the origin of ancient accumulation in the aspect of the terrain landform characteristic , the granularity characteristic and paleoclimate .

  13. 南京汤山葫芦洞碎屑堆积地层对比及地貌演化过程重建

    Comparison of cave deposit stratum and reconstruction of landform evolution in Hulu cave of Tangshan , Nanjing

  14. 风沙地貌是指由于风对地表松散物质的吹蚀、搬运和堆积而形成的地貌。是陆地地貌的重要组成部分。

    Sandstorm landscape is forming of the wind erosing , transport and accumulating surface material of loose sand , which is an important part of the geomorphology of the land .

  15. 据堆积过程,把自然泥石流堆积地貌分为古泥石流台地、老泥石流台地和近代泥石流长柄扇。

    According to the genesis , the accumulational landform of debris flow may be classified into natural and man-made ones .