Estimated seismicity of Venusian wrinkle ridges based on fault scaling relationships
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These files contain all lengths of wrinkle ridges from Bilotti & Suppe (1999), and the code I used to calculate scalar moment release from these faults. We apply segmentation and apply a maximum vertical slip extent. We calculate a moment release rate, or annual moment release, by summing the scalar moments and dividing by a deformation time. The fault lengths are in the last (3rd) column of the Excel file (wrinkleridges_midXY_frank.xlsx) in meters. Please see this reference for more information:<br> Sabbeth, L., Smrekar, S.E., and Stock, J.M. "Estimated seismicity of Venusian wrinkle ridges based on fault scaling<br> relationships." <em>Earth and Planetary Science Letters</em>, 619 (2023): 118308. https://doi.org/10.1016/j.epsl.2023.118308. We develop the method in this paper: https://doi.org/10.1029/2022JE007686



