Major earthquake events can cause ground deformation which can be detectable by GNSS. After a large event, GNSS data can even be used to improve moment magnitude estimations.

For smaller magnitude events, I was wondering what would be the threshold for magnitude/distance from the earthquake source that we can detect the earthquake's coseismic (+postseismic signal) signature on the GNSS time series.

On Nevada Geodetic Laboratory website (http://geodesy.unr.edu/NGLStationPages/stations/LEMN.sta), I saw this formula: "10^(M/2 - 0.79)", we input magnitude (M) to obtain distance value (km). If the distance between the GNSS station and the earthquake epicenter is less than the value we obtained from the formula, it is possible to see a step record on the GNSS time series.

I would really appreciate it if someone could recommend some papers related to this topic.

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