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ECAT (Earthquake Cycle Analyse Toolkits)


A set of tools related to the forward and inverse earthquake cycle.

Continue updating...

  • Stable code will gradually be incorporated
  • New code will gradually be added
  • Bug will gradually be fixed

Installation

  • See Readme Install.md

Coseismic (Uploaded)

Building fault with variance dip angle determined by relocated aftershocks

  1. Case 1: 2021 Maduo earthquake

Image Description

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  1. Case 2: 2023 Kahramanmaraş Türkiye earthquake doublet

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1708350669168

1708435466354

1710499654420

  1. Case 3: 2022 Luding, China earthquake (Pre-Clustering Selection Followed by Fitting)

1709000559665

描述

Building fault with isocurve determined by depth-focused aftershocks

Image Description

1706253529470

Note: Various easy or robust curve fitting methods are only used as a reference to determine the isodepth curve, and ultimately the final fitted curve may need to be extracted based on the user's own background knowledge or visual interaction judgment.

Reference

[1] He, K., Y. Wen, C. Xu, and Y. Zhao (2021), Fault Geometry and Slip Distribution of the 2021 Mw 7.4 Maduo, China, Earthquake Inferred from InSAR Measurements and Relocated Aftershocks, Seismol. Res. Lett., 93(1), 8-20.

[2] He K, Xu C, Wen Y (2022), Coseismic and early post-seismic deformations due to the 2019 earthquake sequence in Ridgecrest, California. Geophysical Journal International, 230(2): 957-975.

[3] jolivetr/csi: Classic Slip Inversion (github.com)

[4] Gmsh 4.11.1

[5] ...

Citation

If you use this package in your research, please cite it as follows:

Kefeng He, Guangyu Xu, Longxiang Sun, Caijun Xu, Yangmao, Wen. (2024). ECAT: Advanced Nonlinear Inversion for Complex Fault Systems (Version 1.1.5). Zenodo. http://doi.org/10.5281/zenodo.13730102

Postseismic (Pending)

  • pscmp_visco_postseismic.py
    • Simple calculating codes about Combined model of viscoelastic relaxation and stress-driven afterslip
  • Deformation components
    • CV (Viscoelastic relaxation due to coseismic): Function cv_cum(t, tobs, disp)
    • AS (Afterslip): Function as_cum(t, disp0, tau_as=0.25, alpha=1.0)
    • AV (Viscoelastic relaxation due to afterslip): Function calAS_AV(pscmpts, obsdate, eqdate, alpha, tau, unit='m', intp_tunit='Y', onlyAV=True, mcpu=4)

Reference

[1] Diao, F., R. Wang, Y. Wang, X. Xiong, and T. R. Walter (2018), Fault behavior and lower crustal rheology inferred from the first seven years of postseismic GPS data after the 2008 Wenchuan earthquake, Earth Planet. Sci. Lett., 495, 202-212, doi:10.1016/j.epsl.2018.05.020.

[2] Diao, F., R. Wang, X. Xiong, and C. Liu (2021), Overlapped Postseismic Deformation Caused by Afterslip and Viscoelastic Relaxation Following the 2015 Mw 7.8 Gorkha (Nepal) Earthquake, J. Geophys. Res.: Sol. Ea., 126(3), doi:10.1029/2020jb020378.

[3] He Ke., Y. Wen, C. Xu, W. Xiong, J. Zang (2023), In preparation.

Interseismic (Pending)

  • pscmp_visco_interseismic.py
    • Calculating velocity related to earthquake cycle
  • Main function
    • calviscoGfromPscmp(pscmpts, T=None, diffint=None, unit='m')

Reference

[1] Diao, F., X. Xiong, R. Wang, T. R. Walter, Y. Wang, and K. Wang (2019), Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS Observations and a Viscoelastic Earthquake‐Cycle Deformation Model, Geophys. Res. Lett., 46(5), 2524-2533, doi:10.1029/2019gl081940.

[2] Zhu, Y., K. Wang, and J. He (2020), Effects of Earthquake Recurrence on Localization of Interseismic Deformation Around Locked Strike‐Slip Faults, J. Geophys. Res.: Sol. Ea., 125(8), doi:10.1029/2020jb019817.

[3] Wang, K., Y. Zhu, E. Nissen, and Z. K. Shen (2021), On the Relevance of Geodetic Deformation Rates to Earthquake Potential, Geophys. Res. Lett., 48(11), doi:10.1029/2021gl093231.