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1)  frequency-space domainτ-p transform
频率空间域τ-p变换
2)  τ-p transform
τ-p变换
1.
2-D prestack migration using double τ-p transform;
双τ-p变换2D叠前偏移
2.
De-aliasing high resolution τ-p transform and its application to wave fields separation;
去假频高分辨率τ-p变换法波场分离
3.
Of all the approaches, the τ-p transform method may be comparatively superior when applied to real siesmic data.
τ-p变换法具有一定的优势、但是,纵、横波的能量在τ-p域往往相互重叠,不容易分开。
3)  τ-p transformation
τ-p变换
4)  τ-p transform
τ-p 变换
1.
Formu- lae for forward and inverse τ-p transform in frequency domain can be obtained by approximating Bessel function in Hankel transform.
正确的点源记录数据平面波分解(τ-p 变换)的数值计算过程包括 Fourier 变换和 Hallkel 变换。
5)  τ–p transform
τ–p变换
1.
Based on previous research results,the theory of extracting transient Rayleigh surface wave using τ–p transform of neighboring trace calculated dispersion curve is described,and the empirical mathematical model considering compactness and velocity of s-wave,and depth is established.
基于前人研究成果,建立了适应于相邻两道计算频散曲线的τ–p变换法提取瞬态瑞雷面波的方法理论,提出了压实度与横波速度和深度之间的经验数学模型。
6)  τ p,τ q
τ-p、τ-q变换
补充资料:变换器式频率表(见交换器式电表)


变换器式频率表(见交换器式电表)
transducer type frequency meter

  曰‘口,”IuullqISn}P旧iUbloo变换器式颇率表meter)(transdueer tyPe见变换器式电表。frequeney
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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