本研究所得出之B、C、D、E類型的頻率範圍與曲線模式，為：（1）B類型反應譜比曲線在0.5∼2Hz 時，比值較小，在2Hz 之後，比值逐漸變大，且在5Hz左右有明顯的峰值出現。（2）C類型反應譜比曲線和B類型相似，只是峰值往低頻移動，大約在3Hz左右。（3）D類型反應譜比曲線峰值出現在2∼3Hz之間，且其比值明顯大於B、C類型的值。（4）E類型反應譜比曲線峰值出現在1.3Hz附近，其比值略小於D類型的值，且峰值的頻帶範圍較D類型來得寬。
由不同頻率的傅氏振幅譜H/V等值圖之分布形態，可得下列結論：（a）大寮到屏東之間：在0.3∼1Hz有明顯的放大效應。（b）屏東平原出海口附近：在0.1∼2Hz有明顯的場址放大效應，2Hz以上逐漸往內陸移動。（c）屏東平原的沖積層厚度由東北往西南邊增厚。（d）高雄市的前鎮、小港附近：在0.5∼1.5Hz有明顯的場址放大。

In this research, we obtained the frequency ranges and curve models of the B, C, D, and E types, and describe them as the following: (1) The Type B curve of H/V response spectral ratio has a smaller value between 0.5 and 2Hz, but gets larger values after 2Hz. Moreover, it has a peak around 5Hz. (2) The Type C curve is similar to that of Type B, but has its peak at around 3Hz. (3) The peak of Type D curve only exhibits between 2 and 3Hz, and its ratio is obviously bigger than those of Types B and C. (4) Type E curve has its peak at around 1.3Hz, and the ratio is smaller than that of Type D. Moreover, it has a wider frequency bandwidth than Type D around the peak.
From the contour of the H/V Fourier spectrum ratio at different frequencies, we got the following conclusions: (a) Between Taliao and Pingtung: it has obvious site amplification exists from 0.3 to 1Hz. (b) Near the seacoast of Pingtung Champaign, obvious magnification of the site effect exists from 0.1 to 2 Hz, and that above 2Hz the contour high area gradually move toward the inland. (c) The thickness of accretion in Pingtung Champaign is getting deeper from the direction of northeast toward southwest. (d) Close to Chienjen and Hsiaokang in Kaohsiung City, there has obvious site amplification effect exists from 0.5 to 1.5Hz.

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