viscous debris flow

基本解释

Intermittent debris flow is the most important moving form of viscous debris flows.
阵流是黏性泥石流的主要运动形式。
Some investigators maintain that large boulders must be supported by turbulence within a viscous debris flow .
有些调查者认为大漂砾是通过粘性泥石流中的涡流搬运的。
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The debris flow gullies of Banzi, Taoguan and Chediguan generate low frequency and low viscous debris flows or hyper-concentrated flows with an average interval of 20~50 years.
板子沟、桃关沟和彻底关沟均为低频率泥石流或高含沙洪水，平均20～50年发生一次；