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应用地球物理  2010, Vol. 7 Issue (4): 325-335    DOI: 10.1007/s11770-010-0257-x
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基于第二代Curvelet变换的面波压制
郑静静1,印兴耀1,张广智1,武国虎2,张作胜2
1. 中国石油大学(华东)地球资源与信息学院,山东东营 257061
2. 胜利物探公司国际部,山东东营 257084
The surface wave suppression using the second generation curvelet transform
Zheng Jing-Jing1, Yin Xing-Yao1, Zhang Guang-Zhi1, Wu Guo-Hu2, and Zhang Zuo-Sheng2
1. Department of Geophysics, China University of Petroleum (East China), Qingdao 266555, China.
2. International Department of Shengli Geophysical Company, Dongying Shandong 257084, China.
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摘要 针对面波能量强、频率低、视速度低等特点,本文提出了基于第二代Curvelet变换的多尺度、多方向分解的面波压制方法,充分利用Curvelet变换的多尺度、多方向功能,分离出含有面波的尺度和方向,然后利用面波与有效波在Curvelet域基本不重叠的特性,进行信噪分离处理。这种方法在实际叠前地震数据的处理中,能够有效压制面波,同时较好地保护有效反射波,特别是反射波的低频分量。文中提出的基于第二代Curvelet变换的去面波方法是一种较好的保幅去噪方法。
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郑静静
印兴耀
张广智
武国虎
张作胜
关键词第二代Curvelet变换   多尺度性   多方向性   面波   去噪     
Abstract: In this paper, we develop a new and effective multiple scale and strongly directional method for identifying and suppressing ground roll based on the second generation curvelet transform. Making the best use of the curvelet transform’s strong local directional characteristics, seismic frequency bands are transformed into scale data with and without noise. Since surface waves and primary reflected waves have less overlap in the curvelet domain, we can effectively identify and separate noise. Applying this method to pre-stack seismic data can successfully remove surface waves and, at the same time, protect the reflected events well, particularly in the low-frequency band. This indicates that the method described in this paper is an effective and amplitude-preserving method.
Key wordsSecond generation curvelet transform   multiscale   strong directional characteristics   surface wave removal   
收稿日期: 2009-12-31;
基金资助:

本研究由国家重点基础研究计划(973)项目(2007CB209605)、国家自然基金项目(40739908)和国家油气重大专项(2008zx05014-001-010hz)资助。

引用本文:   
郑静静,印兴耀,张广智等. 基于第二代Curvelet变换的面波压制[J]. 应用地球物理, 2010, 7(4): 325-335.
ZHENG Jing-Jing,YIN Xing-Yao,ZHANG Guang-Zhi et al. The surface wave suppression using the second generation curvelet transform[J]. APPLIED GEOPHYSICS, 2010, 7(4): 325-335.
 
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