Stretching correction for amplitude-preserving vector wavefield reverse-time migration

Jia-jia Yang; Bing-shou He; Hua-ning Xu; Jun Pan; Jun Liu; Hong Liu

doi:10.31035/cg2018071

2019 Vol. 2, No. 2

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Abstract

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Article navigation > China Geology > 2019 > 2(2): 179-188

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Jia-jia Yang, Bing-shou He, Hua-ning Xu, Jun Pan, Jun Liu, Hong Liu, 2019. Stretching correction for amplitude-preserving vector wavefield reverse-time migration, China Geology, 2, 179-188. doi: 10.31035/cg2018071

Citation:

Jia-jia Yang, Bing-shou He, Hua-ning Xu, Jun Pan, Jun Liu, Hong Liu, 2019. Stretching correction for amplitude-preserving vector wavefield reverse-time migration, China Geology, 2, 179-188. doi: 10.31035/cg2018071

Stretching correction for amplitude-preserving vector wavefield reverse-time migration

a.
Qingdao Institute of Marine Geology, China Geological Survey, Ministry of Natural Resources, Qingdao 266071, China
b.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
c.
Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China

More Information

Corresponding authors: yangjj0714@sina.com (Jia-jia Yang); hebingshou@sina.com (Bing-shou He)

Received Date: 15 October 2018

Revised Date: 30 November 2018

Accepted Date: 07 December 2018

Available Online: 05 June 2019

Publish Date: 25 August 2019

Abstract

Abstract

The migration of multi-wave seismic data is aimed at obtaining the P- and S-wave imaging results of the amplitude preserving. But the P- and S-wave stretching effect produced by the reverse time migration of the elastic wave equation will not only reduce the vertical resolution of the migration results and the amplitude preserving of the large reflection angle. In this paper, the reverse time migration technique of amplitude preserving vector wave-field separating is used. Based on the analysis of the stretch mechanism and the influencing factors of stretch magnitude, the paper gave the stretch correcting factors. Then, realize the stretch correction method at the time that after the reverse extrapolation and before the imaging by solving the problem which is how to calculate the P-wave and Ps-wave propagation directions of imaging points at different times. The stretch correction method can improve the vertical resolution and amplitude fidelity of the imaging results and provide high fidelity input data for seismic data interpretation and inversion.
- reverse-time migration /
- multi-wave and multi-component /
- migration stretch correction /
- amplitude-preserving imaging /
- seismic migration imaging

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