地震烈度包络线通常用地面调查宏观地震影响和破坏现象来划分。
Earthquake isoseismal is usually determined based on the macroscopic earthquake affection and damages observed in the field.
地震烈度包络线通常用地面调查宏观地震影响和破坏现象来划分。
Earthquake isoseismal is usually determined based on the macroscopic earthquake affection and damages observed in the field.
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