洪积平原

  • 网络Alluvial plain;diluvial plain
洪积平原洪积平原
  1. 谈冲、洪积平原粘性土的前期固结压力

    Study of Pre-consolidation Pressure of Cohesive Soil on Alluvial Diluvial Plain

  2. 聚煤环境主要为河流洪积平原的三角洲,扇前湿地环境。

    Coal accumulation environments are mainly the delta of stream-flood plain and marsh .

  3. 准噶尔盆地西北缘洪积平原相油气藏的勘探与开发

    The Rolling Exploration and Development of Flood Plain Reservoir in Northwestern Margin of Junggar Basin

  4. 运城盆地洪积平原全新世环境演变与侵蚀阶段研究

    Holocene Environment Change of Pedogenesis and Erosion phases on Pluvial-alluvial Fan in Yuncheng Basin , Shanxi Province

  5. 提出了干旱内陆河流域冲洪积平原下游区域盐分出路的新思路。

    New thought of flood attack plain downstream district desalting in arid inland river area is given .

  6. 晚更新世以来主要河流阶地形成,其间在0.037Ma前后冲洪积平原形成。

    ; primary river terraces formed since the Late Pleistocene , and diluvium-alluvial plains formed at about 0.037 Ma B.P. .

  7. 太行山前平原动水条件下地下调蓄功能实验研究&以滹沱河冲洪积平原为例

    A study on artificial underground reserve function in the aquifer with river channels in Taihang piedmont plain of China : a case study in the alluvial plain of Hutuo River

  8. 运城市的黄土湿陷性及其深度都要高于临汾地区,特别是在河流高阶地和山前冲洪积倾斜平原区。

    The collapsibility and depth of loess in Yuncheng city is higher than its in Linfen district , especially in the high stream terrace and alluvial-proluvial plain before the mountain forming period .

  9. 应用构造地貌的观点,把太原盆地及其边缘地貌分为:外围断块抬升山地、抬升轻微的丘陵台地、山前堆积的洪积倾斜平原和沉降堆积的冲积平原4种地貌单元。

    Based on the point of tectonic geomorphology , the geomorphology in and outside the Taiyuan Basin were divided into four geomorphologic units : periphery block rising mountain , slightly rising hill tableland , pluvial sedimentation plain , and alluvial sedimentation plain .

  10. 昆仑山前洪积&冲积平原地理环境与地方性氟中毒

    Geographical Environment and Endemic Fluorosis on the Diluvial ─ Alluvial Plain in front of the Kunlun Mountains

  11. 其中河流下游冲洪积三角洲平原、西河河流流经地区以及黑河干流西面的水库区绿洲表现得比较稳定,外围绿洲表现为不够稳定。

    The stable oasis is in alluvial delta plain of Heihe River downstream , West River flow region and the reservoir region of the west of Heihe River .

  12. 地下水体化学特征分异规律为山区裂隙水及山前砾石带重碳酸盐带,山前冲、洪积、湖积平原硫酸盐带,荒漠区及积盐洼地氯化物带。

    For groundwater , they are mountain fissure and piedmont gravel-bicarbonate zone , piedmont diluvial , alluvial and lacustrine plain-sulfate zone and desert salt-accumulating depression-chloride zone .