利用面波衰减的Q模型，反演出近地表的Q值。
Surface wave Q model with attenuation is used to inverse near surface Q value.
这在简单的近地表结构地区或在平原地区可近似认为对地震波场不产生影响。
The seismic wave did not being affected generally in easy near surface or plains region.
这在简单的近地表结构地区或在平原地区可近似认为对地震波场不产生影响。
The seismic wave did not being affected generally in easy near surface or plains region.
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