Abstract
The preferred orientation of clay minerals dominates the intrinsic anisotropy of shale. We introduce the clay lamination (CL) parameter to the Backus averaging method to describe the intrinsic shale anisotropy induced by the alignment of clay minerals. Then, we perform the inversion of CL and the Thomsen anisotropy parameters. The direct measurement of anisotropy is difficult because of the inability to measure the acoustic velocity in the vertical direction in boreholes and instrument limitations. By introducing the parameter CL, the inversion method provides reasonable estimates of the elastic anisotropy in the Longmaxi shale. The clay content is weakly correlated with the CL parameter. Moreover, the parameter CL is abnormally high at the bottom of the Longmaxi and Wufeng Formations, which are the target reservoirs. Finally, we construct rock physics templates to interpret well logging and reservoir properties.
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We are grateful to reviewers for their careful reviews and constructive suggestions.
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The research is supported by the Foundation of State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development (No. G5800-16-ZS-KFZY002), the NSFC and SinoPEC Joint Key Project (No. U1663207), and the National Natural Science Foundation of China (No. 41404090).
Liu Xi-Wu, Professor, Received his Ph.D in Geophysics from Chinese Academy of Sciences. He used to be an associate professor in Geophysics at Ocean University of China from 2004 to 2008. He was a postdoctoral researcher at SinoPEC from 2008 to 2010. He is presently at Exploration and Production Research Institute of SinoPEC, mainly focusing on seismic signal processing, reservoir characterization, seismic fracture characterization, and shale oil/gas geophysical prediction.
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Liu, XW., Guo, ZQ., Liu, C. et al. Anisotropy rock physics model for the Longmaxi shale gas reservoir, Sichuan Basin, China. Appl. Geophys. 14, 21–30 (2017). https://doi.org/10.1007/s11770-017-0609-x
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DOI: https://doi.org/10.1007/s11770-017-0609-x