Cao, F., & Liang, C. (2022). Recent progress on wave gradiometry method. Reviews of Geophysics and Planetary Physics, 54(3), 270–286.

Cao, F., Liang, C., Yang, Y., Zhou, L., Liu, Z., & Liu, Z. (2023). 3D velocity and anisotropy of the southeastern Tibetan plateau extracted by joint inversion of wave gradiometry, ambient noise, and receiver function. Tectonophysics, 848, 229690. https://doi.org/https://doi.org/10.1016/j.tecto.2022.229690

Cao, F., Liang, C., Zhou, L., & Zhu, J. (2020). Seismic Azimuthal Anisotropy for the Southeastern Tibetan Plateau Extracted by Wave Gradiometry Analysis. Journal of Geophysical Research: Solid Earth, 125(5), e2019JB018395. https://doi.org/https://doi.org/10.1029/2019JB018395

Liang, C., Cao, F.*, Liu, Z., & Chang, Y. (2023). A review of the wave gradiometry method for seismic imaging. Earthquake Science36(3), 254–281. https://doi.org/10.1016/J.EQS.2023.04.002

Dai, Y., Liang, C., Cao, F., Chen, L., Liu, Z., Fan, X., & Wang, C. (2024). Decoupled anisotropy in the lower crust and upper mantle extracted by the Wave Gradiometry method resolves the differential deformation mechanisms beneath the northeastern Tibetan Plateau. Earth and Planetary Science Letters, 633, 118654. https://doi.org/https://doi.org/10.1016/j.epsl.2024.118654

Liu, Z., Liang, C., Cao, F., Fan, X., & Chen, C. (2025). Mechanisms for Layered Anisotropy and Anomalous Magmatism of Alaska Subduction System Revealed by Ambient Noise Tomography and the Wave Gradiometry Method. Journal of Geophysical Research: Solid Earth, 130(1). https://doi.org/10.1029/2024JB029105

常英娜, 梁春涛, 曹飞煌 ,周鲁, 廖江涛, 陆威帆, & 王朝亮. (2022). 基于波场梯度法研究安宁河则木河断裂带速度结构. 地球物理学报, 65(8), 2886–2903. https://doi.org/10.6038/cjg2022P0731