Rock Physics Modeling and Seismic AVAZ Responses of Fractured Reservoirs with Different Azimuths-Reference-Cited by-同舟云学术

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Rock Physics Modeling and Seismic AVAZ Responses of Fractured Reservoirs with Different Azimuths

Published:2023-02-14 Issue:3 Volume:180 Page:951-968
ISSN:0033-4553
Container-title:Pure and Applied Geophysics
language:en
Short-container-title:Pure Appl. Geophys.

Author:

Ba Jing,Zhang Wei,Huang Guangtan,Müller Tobias M.,Luo Cong

Funder

National Natural Science Foundation of China

Jiangsu Innovation and Entrepreneurship Plan

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00024-023-03240-y.pdf

Reference45 articles.

1. Afzal, D. M. Z., Atif, R. S., Maryam, T., Ghulam, S., & Bakhtawer, S. (2022). Characterization of seismic anisotropy using azimuthal AVO analysis (AVAz)—An application case study in the deep and tight carbonate reservoirs from Potwar Basin onshore Pakistan. Journal of Applied Geophysics, 205(1), 104767. https://doi.org/10.1016/J.JAPPGEO.2022.104767

2. Al-Marzoug, A. M. (2006). P-wave anisotropy from azimuthal AVO and velocity estimates using 3D seismic data from Saudi Arabia. Geophysics, 71(2), E7–E11. https://doi.org/10.1190/1.2187724

3. Bachrach, R., Sengupta, M., Salama, A., & Miller, P. (2009). Reconstruction of the layer anisotropic elastic parameter and high-resolution fracture characterization from P-wave data: A case study using seismic inversion and Bayesian rock physics parameter estimation. Geophysical Prospecting, 57(2), 253–262. https://doi.org/10.1111/j.1365-2478.2008.00768.x

4. Bahorich, M., & Farmer, S. (1995). 3-D seismic discontinuity for faults and stratigraphic features: The coherence cube. SEG Technical Program Expanded Abstracts, 14(10), 1053–1058. https://doi.org/10.1190/1.1887523

5. Chopra, S., & Marfurt, K. J. (2007). Curvature attribute applications to 3D surface seismic data. The Leading Edge, 26(4), 404–414. https://doi.org/10.1190/1.2723201

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