堆积过程是从浮岩流底部渐进式向前堆积。
The pumice flow deposit begins from its bottom, and gradually develops forward.
利用本文开发的数值模型模拟单一粒径和双粒径混合椭球粒子的随机堆积过程。
The numerical model is applied to simulate the random packing of mono-sized and binary mixtures of ellipsoidal particles.
红粘土的粒度分布表明，东亚冬季风环流而非北半球西风环流控制着红粘土物质的堆积过程。
The size distribution of red clay showed that the accumulation of red clay was controlled by East Asian monsoon circulation rather than westerly circulation.
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