达清夫发现,对于大多数地震来说,震中附近的时间间隔都很短;震中指的是地表上震动最强烈的地方。
For most earthquakes, Wadati discovered, the interval was quite short near the epicenter; the point on the surface where shaking is strongest.
达清夫发现,对于大多数地震来说,震中附近的时间间隔都很短;震中指的是地表上震动最强烈的地方。
For most earthquakes, Wadati discovered, the interval was quite short near the epicenter; the point on the surface where shaking is strongest.
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