Anisotropic Radon Transform and Its Application to Demultiple
Anisotropic Radon Transform and Its Application to Demultiple
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DOI:
10.1002/cjg2.20130
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发表时间:
2014-09
期刊:
影响因子:
--
通讯作者:
Xiang-bo Gong;Han Liguo;Hong-Jian Li
中科院分区:
文献类型:
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作者:
Xiang-bo Gong;Han Liguo;Hong-Jian Li
For the seismic data acquired in the anisotropic medium and with large offset, although we use the high-resolution hyperbolic Radon transform, the energy of the Radon domain is still not convergent. In order to overcome this problem, the influence of the anisotropic factor is considered in the integral path of Radon transform. By introducing the anisotropic anellipticity parameters η from non-hyperbolic moveout formula, the travel-time curve can be accurately described in the horizontal layer for large offset. We derive the integral equation of forward and inverse Radon transform with three parameters, which are the offset, the slowness and the anellipticity. For time-varying of anisotropic Radon transform, the fast algorithm in the frequency domain is not applicable in the process of discretization. This paper adopt the optimal semblance weighted Gauss-Seidel iterative algorithm which not only keeps the high resolution but also has the high calculation efficiency. In the examples of the anisotropic model and real marine seismic data with large offset, this method shows the effective and efficient application to demultiple.