但在低磁纬度地区,作大面积化极换算并进行地质解释的工作仍处于探索阶段。
In area of low magnetic latitude, however, reduction calculation over large data area and geologic interpretation of the resulted data are still in its infancy.
但在低磁纬度地区,作大面积化极换算并进行地质解释的工作仍处于探索阶段。
In area of low magnetic latitude, however, reduction calculation over large data area and geologic interpretation of the resulted data are still in its infancy.
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