河流携带的部分粗砂砾在河床上形成滞留沉积。
Some coarse gravel loaded by the river deposited in the river channel.
采用粒度分析、岩石岩性分析、砾石统计等方法,本文认为新疆叶城地区第四纪粗砂砾层为冲积-洪积类型。
A series of Quaternary sands and gravels are well distributed on the northern foot of West Kunlun Mountains in Yecheng area oi' Xinjiang.
大坝垫层料采用以天然砂砾料为主、掺入小石和粗砂以调整级配的方式生产。
The cushion layer for the dam is constructed with the material prepared mainly with natural sandy gravel and mixed with proper amount of pebble and coarse sand.
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