Directivity in the ruptures of the mainshock (event 4) and the aftershock (event 30), which occured at Goesan, South Korea in 2022. Image is modified from Figure 5a of Lim et al. (JS, 2024, https://doi.org/10.1007/s10950-024-10201-y).
Seismic tomography image slicing the subducting slab (a), mantle wedge (b), and continental crust (c). Image is from Figure 10 of Lim et al. (EPSL, 2018, https://doi.org/10.1016/j.epsl.2018.07.014).
Poroelastic stress model associated with the induced earthquake. Image is from Figure 11 of Lim et al. (JGR, 2020, https://doi.org/10.1029/2019JB019134).
After orientation correction, HT1 is zero, HR3 and HT2 are correlated, and HT2 and HT3 are anticorrelated. HSB is rotated by 145° and 229° in 2005–2007 and 2008–2015, respectively. Image is from Figure S7 of Lim et al. (GJI, 2018, https://doi.org/10.1093/gji/ggx515).