Seismic interpreters commonly pick or interpret seismic data on paper sections along the trough of a wavelet rather than the normally solid-filled peak for ease of viewing.
为了观察方便，地震解释员通常在纸剖面上沿着子波的波谷而不是沿着已涂黑的波峰值来拾取或解释地震资料。
This paper has proposed a hypothesis of magma tides in the asthenosphere to interpret 18.6 year earthquake cycles in major seismic regions of the world which was discovered by the author.
本文提出软流圈岩浆潮的假设来解释作者所发现的全球主要地震区的大地震都存在18.6年地震轮回。
Lateral reservoir prediction using seismic data needs to make seismic data direct correlative with drilling and logging data, then to comprehensively interpret rock formations.
利用地震资料进行储层横向预测，是先将地震资料变成可与钻井、测井资料直接对比的形式，然后以岩层为单元进行综合解释。
Although one can get full acoustic wave data using acoustic wave equation for seismic modeling, the data are difficult to interpret for the multiples.
利用全声波方程进行地震波场的数值模拟，虽然可以计算全声波波场值，但是也常常会出现层间多次波，给资料解释造成一定的困难。
The theoretical model and actual calculated results show that the seismic coal thickness assistant interpretation system can be used to interpret coal thickness and has better geological results.
理论模型和实际资料试算结果表明：利用该系统进行煤层厚度解释，得到了较好的地质效果。
Studies of seismic anisotropy in the crust and mantle are of wide application and scientific implication in geodynamics, which could interpret much geological and geophysical problem.
地壳与上地幔各向异性研究在地球动力学领域有广泛的应用和重要的科学意义，其研究有助于许多地质和地球物理基本问题的解释。
Studies of seismic anisotropy in the crust and mantle are of wide application and scientific implication in geodynamics, which could interpret much geological and geophysical problem.
地壳与上地幔各向异性研究在地球动力学领域有广泛的应用和重要的科学意义，其研究有助于许多地质和地球物理基本问题的解释。
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