Table 1 Correction coefficient \(\beta\) used to balance the seismic moment calculated from geodetic strain rates to that of past large earthquakes

\(\dot{\gamma }\)

(Eq. 1)

\(\mathrm{Max}(\left|{\dot{\varepsilon }}_{h1}\right|, \left|{\dot{\varepsilon }}_{h2}\right|)\)

(Eq. 2)

\(\mathrm{Max}(\left|{\dot{\varepsilon }}_{h1}\right|, \left|{\dot{\varepsilon }}_{h2}\right|, \left|{\dot{\varepsilon }}_{h1}+{\dot{\varepsilon }}_{h2}\right|)\)

(Eq. 3)