这表明在低应力区，冰体流动更接近牛顿流体。
We assume that the glacier ice is a Newton fluid in the low stress region.
多数断层两侧一定范围内以及断层内部是相对的低应力区。
In areas on both sides of faults and within the interior of faults, stresses are usually lower than the regional stress.
在有些结构中停滞在低应力区的裂纹起着降低约束的作用。
In some structures the cracks arrested in low stress areas served to relieve the restraint condition.
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