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角度域共成像点道集剩余曲率法偏移速度分析(英文)

Residual curvature migration velocity analysis for angle domain common imaging gathers

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【作者】 张凯李振春曾同生董晓春

【Author】 Zhang Kai1,Li Zhen-Chun1,Zeng Tong-Sheng1,and Dong Xiao-Chun2 1.College of Earth Resources and Information in China University of Petroleum,Qingdao 266555,China.2.Department of Quality and Energy Conservation of PetroChina Jilin Oilfield Company,Songyuan 138000,China.

【机构】 中国石油大学(华东)地球资源与信息学院地球物理系中国石油吉林油田公司质量节能处

【摘要】 叠前深度偏移速度分析是地震数据处理方法研究的重点,是影响地震成像效果的关键技术之一。本文的基于角度域共成像点道集剩余曲率的偏移速度分析方法,旨在通过角度域共成像点道集(ADCIGs)来建立局部入射角与偏移深度之间的联系,通过角度道集剩余速度分析来修正、更新偏移速度。不同于偏移距域共成像点道集(ODCIGs),ADCIGs较少地受到由于多路径问题而产生的波场干涉假象的影响,更适合于偏移速度分析。本文在推导出基于ADCIGs的水平地层深度剩余量公式的基础上,提出了基于ADCIGs的沿层扫描法速度更新流程,凹陷模型和实际资料的试处理表明了本方法的正确性和有效性。

【Abstract】 Pre-stack depth migration velocity analysis is one of the keys to influencing the imaging quality of pre-stack migration.In this paper we cover a residual curvature velocity analysis method on angle-domain common image gathers(ADCIGs) which can depict the relationship between incident angle and migration depth at imaging points and update the migration velocity.Differing from offset-domain common image gathers(ODCIGs),ADCIGs are not disturbed by the multi-path problem which contributes to imaging artifacts,thus influencing the velocity analysis.On the basis of horizontal layers,we derive the residual depth equation and also propose a velocity analysis workflow for velocity scanning.The tests to synthetic and field data prove the velocity analysis methods adopted in this paper are robust and valid.

【基金】 supported by the National 863 Program (Grant No.2006AA06Z206,Sustained supported);the National Science and Technology Major Project (Grant No.2008ZX05006-004);SinoPec Group Marine Facies Research (Grant No.08370502000410)
  • 【文献出处】 Applied Geophysics ,应用地球物理(英文版) , 编辑部邮箱 ,2010年01期
  • 【分类号】P631.44
  • 【被引频次】19
  • 【下载频次】284
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