在大部分金属中，行列可以很容易的相互滑动，这一特性会降低金属的总强度。
In most metals these rows can readily slip past one another, a characteristic that will lower the overall strength of the material.
模拟地磁总强度的形态为近直线型，而数字化地磁总强度则有显著的日动态变化。
The change shapes of the imitative data of the geomagnetic total intensity shows a straight line and the one of the digital data appears a daily change.
通过对区域前兆原始观测数据的处理，突出了这次地震前的应变和地磁总强度短临前兆异常信息。
By processing data of precursory earthquakes, we try to find the useful anomaly information from the data of strain and total geomagnetism intensity.
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