高频的频率边带由于幅度交叠的部分较少，所以对强度起伏贡献较少。
The higher frequency sidebands would have less contribution to the fluctuation due to smaller amplitude overlapping.
结果表明，菲律宾海和南海显示了与磁条带、扩张脊对应或斜交的高频成分大地水准面起伏条带。
The results show that within the Philippine Sea and the South China Sea, short - wavelength lineations of the geoid undulation are parallel or cross to magnetic lineations and rifting ridges.
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