Noise has traditionally been suppressed or eliminated in seismic data sets by the use of Fourier filters and,to a lesser degree,nonlinear statistical filters.Although these methods are quite useful under specific conditions,they may produce undesirable effects for the low signal to noise ratio data.In this paper,a new method,multi-scale ridgelet transform,is used in the light of the theory of ridgelet transform.We employ wavelet transform to do subband decomposition for the signals and then use non-linear thresholding in ridgelet domain for every block.In other words,it is based on the idea of partition,at sufficiently fine scale,a curving singularity looks straight,and so ridgelet transform can work well in such cases.Applications on both synthetic data and actual seismic data from Sichuan basin,South China,show that the new method eliminates the noise portion of the signal more efficiently and retains a greater amount of geologic data than other methods,the quality and consecutiveness of seismic event are improved obviously as well as the quality of section is improved. Noise has traditionally been suppressed or eliminated in seismic data sets by the use of Fourier filters and, to a lesser degree, nonlinear statistical filters. Although these methods are quite useful under specific conditions, they may produce undesirable effects for the low signal to noise ratio data.In this paper, a new method, multi-scale ridgelet transform, is used in the light of the theory of ridgelet transform. We employ wavelet transform to do subband decomposition for the signals and then use non-linear thresholding in ridgelet domain for every block.In other words, it is based on the idea of ​​partition, at sufficiently fine scale, a curving singularity looks straight, and so ridgelet transform can work well in such cases. Applications on both synthetic data and actual seismic data from Sichuan basin , South China, show that the new method eliminates the noise portion of the signal more efficiently and retains a greater amount of geologic data than other methods, the quality and consecutivenes s of seismic events are improving obviously as well as the quality of section is improved.