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Seismic data separation of simultaneous source based on an improved iterative denoising method |
Jian-Hong GUO1,2, Jing-Wang CHENG3( ), Zhi-Ruo CHEN2, Bing YANG1,2, Hao YAN4 |
1. Geophysics and Oil Resource Institute,Yangtze University,Wuhan 430100,China 2. Key Laboratory of Exploration Technologies for Oil and Gas Resources,Ministry of Education,Yangtze University,Wuhan 430100,China 3. College of Mining Engineering,Taiyuan University of Technology,Taiyuan 030024,China 4. Tianjin Branch of CNOOC Ltd.,Tianjin 300452,China |
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Abstract Compared with single source acquisition method,simultaneous source acquisition technology can greatly increase field acquisition efficiency,and the separation of blended data is the key.When pseudo-segregated records of mixed simultaneous source data are sorted from common gathers to other gathers,the seismic signals of secondary sources show random noise,which can be separated by iterative denoising method.In this paper,the traditional iterative prediction denoising method is improved by adding the last separation result before each denoising to increase the stability of the iterative denoising,and combining with Multidirectional Vector Median Filtering to remove random noise.Through the separation test of simultaneous source mixed data of theoretical model,it is shown that the proposed method has better separation effect and is more robust,and can be operated under the condition of different parameters and maintain certain stability.Finally,the method is applied to the separation of Simultaneous Source Marine Line data,and a better separation result can be obtained.The method has practical application value.
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Received: 18 January 2019
Published: 25 October 2019
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Corresponding Authors:
Jing-Wang CHENG
E-mail: chjw2008@126.com
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Common offset gather contrast picture a—traditional single source gather;b—multi-source blended excitation gather
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Blended excitation mode and shot time a—blended mode;b—random excitation of multiple sources
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Common-shot gather seismic record a—the 50th single source;b—the 110th single source;c—the 50th blended source
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Comparison of denoising results of common detection point gathers a—iterative prediction subtraction method(the main source);b—the method of this paper(the main source);c—iterative prediction subtraction method(the secondary source);d—the method of this paper(the secondary source)
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Signal-noise ratio iterative curve a—signal-noise ratio of the main source after separation;b—signal-noise ratio of the secondary after separation
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| 滤波时窗 长度 | 地震 道数 | 中值滤波矢量 方向范围 | 迭代二十次信噪比/dB | 迭代预测相减 | 本文改进方法 | 主震源 | 次震源 | 主震源 | 次震源 | 第一组 | 5 | 5 | 5 | 14.0125 | 12.2117 | 15.9059 | 15.7402 | 第二组 | 7 | 7 | 10 | 13.0922 | 10.9931 | 15.7113 | 15.2896 | 第三组 | 9 | 7 | 15 | 11.9421 | 10.1104 | 14.4596 | 14.2067 |
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Comparison of denoising results with different filtering parameters
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Comparison of separation effect of blended excitation a—comparison of signal-noise ratio of the main source;b—comparison of signal-noise ratio of the secondary
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The separation results of fiftieth blended source a—the 50th signal source record separated by this paper method;b—the 110th signal source record separated by this paper method;c—the 50th signal source record separated by regular method;d—the 110th signal source record separated by regular method
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Blended acquisition technique for offshore multiple seismic sources a—actual data of offshore single source excitation;b—blended multi-source data(top 3000 time windows)
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The thirty-second common offset gather and denoising results a—the main source common offset gather;b—denoising results for figure a;c—the secondary source common offset gather;d—denoising results for figure c
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Separation record of actual blended source a—the main source after separation of the 32nd blended source;b—the secondary source after separation of the 32nd blended source
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Comparison of Separation record of actual blended source a—partial data of single source excitation at sea 32nd blended source;b—partial data after separation of 32nd blended source
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