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基于共散射道集的叠前时间偏移/反偏移提高叠前数据质量
引用本文:孙小东,宋煜,李振春. 基于共散射道集的叠前时间偏移/反偏移提高叠前数据质量[J]. 地球物理学进展, 2020, 0(4): 1454-1458
作者姓名:孙小东  宋煜  李振春
作者单位:深层油气重点实验室;山东省油藏地质重点实验室
基金项目:国家自然科学基金(41574098,41630964);中央高校基本科研业务费专项资金(18CX02059A);深层油气重点实验室开发基金(20CX02111A);中国石化地球物理重点实验室开放基金项目(wtyjy-wx2018-01-07);中石油重大科技项目“塔里木盆地深层复杂高陡构造与碳酸盐岩储层地震速度建模及成像关键技术”(ZD2019-183-003)联合资助。
摘    要:
为了提高叠前数据质量,将叠前时间偏移/反偏移与共散射点道集相结合,提出了一种新的时间偏移/反偏移方法.利用改进的CRS参数建立精确的速度模型,提高偏移成像质量.将振幅映射到共偏移距顶点来生成共散射点道集,将偏移和中点上的多参数叠加,通过叠加数据,实现了叠前数据增强,道集的数量远高于传统叠前时间偏移的叠加数量.利用基于中点位移、半偏移距和偏移速度的算子进行反偏移处理,能量重新分配回时间域中的每个绕射同相轴,压制噪声,地震资料信噪比和成像精度均得到了提高.提高质量后的叠前数据可用于后续的速度分析、叠加、偏移等常规处理中,效果好于原始CMP道集.模型和实际数据的计算结果均验证了该方法的正确性和有效性,该方法在低信噪比资料的处理中将会有广阔的应用前景.

关 键 词:共散射点道集  叠前时间偏移  反偏移  改进CRS算子

Prestack time migration/demigration based on common scattered gather improves the quality of prestack data
SUN Xiao-dong,SONG Yu,LI Zhen-chun. Prestack time migration/demigration based on common scattered gather improves the quality of prestack data[J]. Progress in Geophysics, 2020, 0(4): 1454-1458
Authors:SUN Xiao-dong  SONG Yu  LI Zhen-chun
Affiliation:(Key Laboratory of Deep Oil and Gas,China University of Petroleum(East China),Qingdao 266580,China;Shandong Provincial Key Laboratory of Reservoir Geology,China University of Petroleum(East China),Qingdao 266580,China)
Abstract:
In order to improve the quality of pre-stack data,a new time domain migration/premigration method is proposed by combining the prestack time migration/premigration with Common Scatter points.The improved CRS parameters are used to establish an accurate velocity model,which improves the accuracy of time migration.By mapping the amplitude to the common offset vertex to generate the common scattering point trace set,the multiple parameters on the offset and midpoint are superimposed,and the prestack data is enhanced by superimposing the data.The number of trace sets is much higher than that of traditional pre-stack time migration.By using the operators based on mid-point displacement,half-offset and migration velocity,the energy is redistributed back to each diffraction in-phase axis in the time domain,the noise is suppressed,and the signal-to-noise ratio and imaging accuracy of seismic data are improved.The improved prestack data can be used in subsequent conventional processing such as velocity analysis,stack and migration,and the result is better than the original CMP data set.The correctness and validity of this method have been verified by the model and the calculation results of the actual data.
Keywords:Common scatter point gather  Prestack time migration  Inverse migration  Improved CRS operator
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