Articles | Volume 16, issue 4/5
https://doi.org/10.5194/se-16-391-2025
https://doi.org/10.5194/se-16-391-2025
Research article
 | 
19 May 2025
Research article |  | 19 May 2025

The 3D QP model of the China Seismic Experimental Site (CSES-Q1.0) and its tectonic implications

Mengqiao Duan, Lianqing Zhou, Ying Fu, Yanru An, Jingqiong Yang, and Xiaodong Zhang

Related authors

OpenSWI: A Massive-Scale Benchmark Dataset for Surface Wave Dispersion Curve Inversion
Feng Liu, Sijie Zhao, Xinyu Gu, Fenghua Ling, Peiqin Zhuang, Yaxing Li, Rui Su, Lihua Fang, Lianqing Zhou, Jianping Huang, and Lei Bai
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-502,https://doi.org/10.5194/essd-2025-502, 2025
Preprint under review for ESSD
Short summary

Cited articles

Bai, D., Unsworth, M. J., Meju, M. A., Ma, X., Teng, J., Kong, X., Sun, Y., Sun, J., Wang, L., Jiang, C., Zhao, C., Xiao, P., and Liu, M.: Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging, Nat. Geosci., 3, 358–362, https://doi.org/10.1038/ngeo830, 2010. 
Bao, X., Sun, X., Xu, M., Eaton, D. W., Song, X., Wang, L., Ding, Z., Mi, N., Li, H., Yu, D., Huang, Z., and Wang, P.: Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions, Earth Planet. Sci. Lett., 415, 16–24, https://doi.org/10.1016/j.epsl.2015.01.020, 2015. 
Bao, X., Song, X., Eaton, D. W., Xu, Y., and Chen, H.: Episodic Lithospheric Deformation in Eastern Tibet Inferred From Seismic Anisotropy, Geophys. Res. Lett., 47, e2019GL085721, https://doi.org/10.1029/2019GL085721, 2020. 
Brune, J. N.: Tectonic stress and the spectra of seismic shear waves from earthquakes, J. Geophys. Res., 75, 4997–5009, https://doi.org/10.1029/JB075i026p04997, 1970. 
CENC: The earthquake catalogues and phase reports. China Earthquake networks center, National Earthquake Data Center, http://data.earthquake.cn (last access: January 2025), 2025. 
Download
Short summary
We obtain the highest-resolution three-dimensional P-wave attenuation model in the China Seismic Experimental Site to date. The P-wave attenuation value anomalies along large fault zones, some basin areas, and the Tengchong volcanic area are low, reflecting the high degree of medium fragmentation in these areas with thick sedimentary layers or rich in fluids.
Share