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首頁» 往期文章» 2014» Issue 3» 石油地質與地球物理

Petroleum Science >2014,??Issue 3:??376-384 DOI: https://doi.org/10.1007/s12182-014-0351-4

Seismic energy dispersion compensation by multi-scale morphology Open?Access

文章信息

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作者：Yu Junqing,Wang Runqiu,Liu Taoran,Zhang Zhenglong,Wu Jian,Jiang Yongyong,Sun Lipeng and Xia Pei
作者單位：

College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;BGP Research & Development Center, Hebei 072751, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China;College of Geophysics and Information Engineering, China University of Petroleum (Beijing), Beijing 102249, China

投稿時間：2013-04-06
引用方式：Yu, J., Wang, R., Liu, T. et al. Pet. Sci. (2014) 11: 376. https://doi.org/10.1007/s12182-014-0351-4

文章摘要

Seismic energy decays while propagating subsurface, which may reduce the resolution of seismic data. This paper studies the method of seismic energy dispersion compensation which provides the basic principles for multi-scale morphology and the spectrum simulation method. These methods are applied in seismic energy compensation. First of all, the seismic data is decomposed into multiple scales and the effective frequency bandwidth is selectively broadened for some scales by using a spectrum simulation method. In this process, according to the amplitude spectrum of each scale, the best simulation range is selected to simulate the middle and low frequency components to ensure the authenticity of the simulation curve which is calculated by the median method, and the high frequency component is broadened. Finally, these scales are reconstructed with reasonable coefficients, and the compensated seismic data can be obtained. Examples are shown to illustrate the feasibility of the energy compensation method.

關鍵詞

    Seismic wave, multi-scale morphology, dispersion compensation, high resolution, median method, spectrum simulation