Least-squares reverse time migration method using the factorization of the Hessian matrix
Sun Xiao-Dong 1,2, Teng Hou-Hua♦3 , Ren Li-Juan 4, Wang Wei-Qi 1, and Li Zhen-Chun 1
1. Key Laboratory of Deep Oil& gas, China University of Petroleum (East China), Qingdao, 266580;
2. Shandong Provincial Key Laboratory of Reservoir Geology, China University of Petroleum (East China), Qingdao,266580.
3. Geophysical Research Institute of SINOPEC Shengli Oilfi eld, Dongying, 257022;
4. Zhanjiang Branch of CNOOC (China) Co., Ltd, Zhanjiang, 524000.
Abstract Least-squares reverse time migration (LSRTM) can eliminate imaging artifacts in an iterative way based on the concept of inversion, and it can restore imaging amplitude step by step. LSRTM can provide a high-resolution migration section and can be applied to irregular and poor-quality seismic data and achieve good results. Steeply dipping reflectors and complex faults are imaged by using wavefield extrapolation based on a two-way wave equation. However, the high computational cost limits the method’s application in practice. A fast approach to realize LSRTM in the imaging domain is provided in this paper to reduce the computational cost significantly and enhance its computational efficiency. The method uses the Kronecker decomposition algorithm to estimate the Hessian matrix. A low-rank matrix can be used to calculate the Kronecker factor, which involves the calculation of Green’s function at the source and receiver point. The approach also avoids the direct construction of the whole Hessian matrix. Factorization-based LSRTM calculates the production of lowrank matrices instead of repeatedly calculating migration and demigration. Unlike traditional LSRTM, factorization-based LSRTM can reduce calculation costs considerably while maintaining comparable imaging quality. While having the same imaging effect, factorizationbased LSRTM consumes half the running time of conventional LSRTM. In this regard, the application of factorization-based LSRTM has a promising advantage in reducing the computational cost. Ambient noise caused by this method can be removed by applying a commonly used filtering method without significantly degrading the imaging quality.
The research gets funded by the National Natural Science Foundation of China (No.41574098 & 41630964), the Fundamental Research Funds for the Central Universities (No.18CX02059A), the Development Fund of Key Laboratory of Deep Oil & Gas (No. 20CX02111A), SINOPEC Key Laboratory of Geophysics open fund (No. wtyjy-wx2018-01-07), Shandong Natural Science Foundation of China (No. ZR2020MD048) and the Major Scientific and Technological Projects of CNPC (No. ZD2019-183-003).
Corresponding Authors: Teng Hou-Hua (E-mail:544203089@qq.com).
E-mail: 544203089@qq.com
About author: Sun Xiao-Dong (doctor) is working as a lecturer in the Department of Applied Geophysics at the China University of Petroleum (East China). His research interests include wave propagation, inversion, and imaging. sunxd@upc.edu.cn
Cite this article:
. Least-squares reverse time migration method using the factorization of the Hessian matrix[J]. APPLIED GEOPHYSICS, 2021, 18(1): 94-100.
2021, Vol. 18 
