这里的地形地貌、重力异常和磁异常沿东方向呈条带状分布。
We recognized that the geomorphology, gravity and magnetic anomalies trend ne direction as bandings.
由于受古地形及沉积物源的控制，砂体沿北东南西向呈条带状分布。
Controlled by paleotopography and sediment source, sand bodies had a banding distribution along the northeast-southwest direction.
因铁路是条带状分布的，一条长大铁路有可能涉及到不同地区的工程地质问题。
Because 'of the strip distribution, a long railway may meet different questions indifferent areas.
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