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Prestack four-parameter synchronous inversion method based on viscoelastic medium theory and its applications |
LIU Hao-Jie1, CHEN Yu-Mao1, WANG Yan-Guang1, ZONG Zhao-Yun2, WU Guo-Chen2, HOU Qing-Jie1,3 |
1. Geophysical Research Institute,Sinopec Shengli Oilfield Company,Dongying 257022,China 2. School of Geosciences,China University of Petroleum,Qingdao 266580,China 3. Working Station for Postdoctoral Scientific Research,Shengli Oilfield,Dongying 257000,China |
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Abstract Prestack seismic data contain elastic and viscoelastic information such as P-wave velocity,S-wave velocity,density and absorption attenuation parameters,among which absorption attenuation property is particularly sensitive to reservoir physical properties and fluid properties.Based on the accurate Zoeppritz equation of viscoelastic medium and the theory of medium decomposition,the authors established the characteristic equation of P-wave reflection coefficient including P-wave velocity,S-wave velocity,density and absorption attenuation parameters.Furthermore,under the constraint of Bayesian inversion framework,the simultaneous inversion of prestack four parameters was realized.The reliability of the method was verified by the trial of forward model.Finally,the method was applied to oil and gas identification in the eastern offshore exploration area of the Shengli Oilfield.Compared with things of the fluid factor based on elastic medium,the absorption and attenuation parameters obtained by the four-parameter simultaneous inversion method can more accurately characterize the distribution of oil and gas.
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Received: 09 October 2019
Published: 01 March 2021
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Variation of reflection coefficient of first type AVO longitudinal wave with incident angle a—Qp=10;b—Qp=20;c—Qp=50;d—figure a local enlarged;e—figure b local enlarged;f—figure c local enlarged
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Flow chart of synchronous inversion method based on prestack four parameters of viscoelastic medium
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Forward modeling parameters of Marmousi2 model a—P wave velocity;b—S wave velocity;c—density;d—Q value
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Simultaneous inversion results of four parameters of Marmousi2 model a—P wave velocity;b—S wave velocity;c—density;d—Q value
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Seismic profile and prestack inversion profile of actual work area a—seismic profile;b—clastic inversion fluid factor;c—absorption and attenuation parameter
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Cross section of absorption attenuation parameters in actual work area a—connecting section of fault uplifted side;b—connecting section of fault downthrow side
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Simultaneous inversion of four parameters along NgI horizon in actual work area a—P wave velocity;b—S wave velocity;c—density;d—absorption and attenuation parameters
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