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Wave field analysis and imaging of near-surface scatterings |
Peng-Peng PENG1,2, Cheng-Yu SUN1, Zhen Ma1, Wen-Jing LI1,3 |
1. School of Geosciences,China University of Petroleum,Qingdao 266580,China 2. Ya'an Bureau of Land and Resources,Ya'an 625000,China 3. Research & Development Center of BGP,Zhuozhou 072751,China; |
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Abstract Studying the basic characteristics of near-surface scattering waves and determining the location of near-surface heterogeneities help seismic imaging,survey planning,and avoiding geological disasters.In order to study the wave fields characteristics of near-surface heterogeneous bodies,the authors used the high-order finite difference numerical simulation technique and perturbation theory method to simulate the wave field records of shallow surface scatters and analyze the basic characteristics of near-surface scattering waves.The near surface heterogeneity was located by introducing of reverse time migration imaging technology with the scattering wave field as an extrapolated wave field.The numerical results indicate that surface-wave scatterings are usually stronger than those body-wave scatterings and that forward scatterings are also stronger than backward scatterings.Moreover,near-surface scatters can be precisely imaged by the elastic wave reverse time migration.The near-surface scatters can be regarded as a secondary source,which increases the near-surface illumination.Using the scattered wave field can improve the accuracy of near-surface velocity inversion and seismic imaging.
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Received: 08 March 2018
Published: 24 October 2018
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模型 | | 层厚(直径)/m | vp/(m/s) | vs/(m/s) | 密度/(kg/m3) | | 第1层 | 10 | 800 | 200 | 2000 | 模型1 | 第2层 | 90 | 1200 | 600 | 2000 | | 散射体 | 4 | 600 | 100 | 2000 | | 第1层 | 200 | 1800 | 1000 | 1750 | 模型2 | 第2层 | 200 | 3000 | 1500 | 2250 | | 散射体 | 20 | 2500 | 1200 | 2000 |
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| 层厚(直径)/m | vp/(m/s) | vs/(m/s) | 密度/(kg/m3) | 第1层 | 50 | 1800 | 1000 | 1750 | 第2层 | 150 | 3000 | 1500 | 2250 | 散射体 | 10 | 3000 | 1500 | 2250 |
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