Cite
Elastic Wave Velocity Changes Due to the Fracture Aperture and Density, and Direct Correlation With Permeability: An Energetic Approach to Mated Rock Fractures.
MLA
Sawayama, K., et al. “Elastic Wave Velocity Changes Due to the Fracture Aperture and Density, and Direct Correlation With Permeability: An Energetic Approach to Mated Rock Fractures.” Journal of Geophysical Research. Solid Earth, vol. 127, no. 2, Feb. 2022, pp. 1–17. EBSCOhost, https://doi.org/10.1029/2021JB022639.
APA
Sawayama, K., Ikeda, T., Tsuji, T., Jiang, F., Nishizawa, O., & Fujimitsu, Y. (2022). Elastic Wave Velocity Changes Due to the Fracture Aperture and Density, and Direct Correlation With Permeability: An Energetic Approach to Mated Rock Fractures. Journal of Geophysical Research. Solid Earth, 127(2), 1–17. https://doi.org/10.1029/2021JB022639
Chicago
Sawayama, K., T. Ikeda, T. Tsuji, F. Jiang, O. Nishizawa, and Y. Fujimitsu. 2022. “Elastic Wave Velocity Changes Due to the Fracture Aperture and Density, and Direct Correlation With Permeability: An Energetic Approach to Mated Rock Fractures.” Journal of Geophysical Research. Solid Earth 127 (2): 1–17. doi:10.1029/2021JB022639.