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solifluction
英 [ˈsɒlɪˌflʌkʃ(ə)n] 美 [ˌsɑːləˈflʌkʃn]

  • n. [地质] 泥流；融冻泥流；[地质] 泥流作用

专业释义英英释义

  • 泥流
    融冻泥流
    土流
    冻融泥流
  • 融冻泥流

·2,447,543篇论文数据，部分数据来源于NoteExpress

Solifluction

  • abstract: In geomorphology, solifluction is a slow mass wasting slope process, occurring in periglacial environments. Solifluction describes the slow downslope movement of water-saturated sediment due to recurrent freezing and thawing of the ground, affected by gravity.

以上来源于: WordNet

 柯林斯英汉双解大词典 

solifluction (also solifluxion)

  • 1. 

    N slow downhill movement of soil, saturated with meltwater, over a permanently frozen subsoil in tundra regions 泥流作用

同近义词

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