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声介质波动方程反射旅行时反演方法
引用本文:付继有,李振春,杨国权,张凯,刘玉金,谢亚妮.声介质波动方程反射旅行时反演方法[J].石油地球物理勘探,2015,50(6):1134-1140.
作者姓名:付继有  李振春  杨国权  张凯  刘玉金  谢亚妮
作者单位:1.中国石油大学(华东)地球科学与技术学院, 山东青岛 266580;2.中国石化石油勘探开发研究院, 北京 100083;3.中国石油塔里木油田分公司勘探开发研究院, 新疆库尔勒 841000
基金项目:本项研究受国家自然科学基金项目(41204086,41374122)、国家科技重大专项课题(2011ZX05006-002)及山东省自然科学基金项目(ZR2013DL012)联合资助。
摘    要:储层精细描述需要精准的背景速度场,全波形反演(FWI)能求取浅层速度场高波数成分。透射波和折射波一般具有较大入射角孔径,可用来恢复速度模型的长波长分量;反射波仅有较小反射角孔径,通常用于恢复速度场短波长分量。本文利用偏移/反偏移算子从背景速度场获取反射波信息,推导了反射波路径;进而得到了波动方程反射层析梯度公式;反演过程中结合Ma和Luo的思路改进了反射层析中伴随源的形式,并修改了梯度的计算;运用动态图像校正法计算反射波旅行时差,实现了利用反射波信息反演速度场低波数成分。模型试算结果表明,本文方法能提高反演的稳定性,具有更好应用潜力。

关 键 词:反射旅行时反演  反偏移  动态图像校正  反射波路径  光滑背景速度  全波形反演  
收稿时间:2014-09-13

Wave equation reflection travel-time inversion in acoustic media
Fu Jiyou,Li Zhenchun,Yang Guoquan,Zhang Kai,Liu Yujin,Xie Yani.Wave equation reflection travel-time inversion in acoustic media[J].Oil Geophysical Prospecting,2015,50(6):1134-1140.
Authors:Fu Jiyou  Li Zhenchun  Yang Guoquan  Zhang Kai  Liu Yujin  Xie Yani
Affiliation:1. School of Geosciences, China University of Petroleum(East China), Qingdao, Shandong 266580, China; 2. Research Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083, China; 3. Research Institute of Petroleum Exploration and Development, Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China
Abstract:The key of reservoir characterization needs accurate background velocity field. Full waveform inversion(FWI) can recover higher wave number information of shallow layers. Transmitted wave and refracted wave usually have a larger incidence angle aperture; they can be used to recover the long wavelength components of the velocity model. While reflections have narrow incidence angle aperture, they are used to recover short wavelength components. Therefore, we rebuilt the reflections gradient to recover velocity model long wavelength components. We get reflections from the background velocity field using migration and demigration operators and construct the reflected wave paths. Then we establish a gradient formula of wave equation reflection travel-time inversion. During inversion process, we combine the ideas of Ma and Luo to improve the form of adjoint sources. We also modify the gradient formulation. Simultaneously dynamic image warping method is used for the time lag calculation between reflections. Finally we achieve a low wavenumber components inversion of velocity model using reflected wave information. Model tests demonstrate better stability and application potentiality of the proposed method.
Keywords:reflections travel-time inversion  demigration  dynamic image warping  reflected wave paths  smooth background velocity  full-waveform inversion(FWI)  
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