本文提出的“射线参数法”，可由多道地震记录谱直接估算层速度或层速度线性梯度值。
A new method, the ray parameter method, is presented in this paper to derive velocity - or its linear gradient-depth information, directly from multi-channel seismic data.
利用唐山近场强震记录对如何分析场地反应进行研究，分析比较了多种方法：线性反演法、传统的谱比法以及接收函数法。
We compared site response from the S wave inversion and those from other techniques, such as traditional direct spectral ratios of S waves and receiver function of S waves.
采用眼动记录法，探讨了工作记忆、两个前提间的关系以及表达方式对线性三段论推理的影响。
Using ASL 504 Model eye-tracker system, we investigated working memory, premises relationship and the affirmative or negative premises influences on the linear syllogism problems solving.
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