1) τ p,τ q
τ-p、τ-q变换
2) τ-q transform
τ-q变换
1.
We improve the τ-p transform methods and propose what we call τ-q transform method.
文中在τ-p变换的基础上对波场分离方法作了改进,提出一种经坐标拉伸的τ-p变换法,称为τ-q变换。
3) 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。
5) 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。
6) 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。
补充资料：τ系数
见社会统计学。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条