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本文指出,文献[1]关于“在地表地震磁异常的全域内,总强度的变化不能为零,其变化幅度△F与垂直分量的变化幅度△Z应是大体相当”的论断不是普遍成立的.因此,不应忽视对分量的观测.
This paper points out that it is not generally accepted in [1] that “the change of total intensity can not be zero in the whole region of the magnetic anomaly of the surface earthquakes, and the change range ΔF and the vertical component △ Z should be roughly equivalent” Therefore, the observation of the components should not be ignored.