The centroid moment tensor solution of the 23 June 2020 M_W7.4 Mexico earthquake

Zhang Z,Xu L S. 2020. 2013 M_W7.8 South Scotia Ridge earthquake:Focal mechanism inversion of the multi-point source[J]. Chinese Journal of Geophysics,63(8):2978–2998.

Duputel Z,Rivera L,Kanamori H,Hayes G. 2012. W phase source inversion for moderate to large earthquakes (1990−2010)[J]. Geophys J Int,189(2):1125–1147. doi: 10.1111/j.1365-246X.2012.05419.x

Dziewonski A M,Chou T A,Woodhouse J H. 1981. Determination of earthquake source parameters from waveform data for studies of global and regional seismicity[J]. J Geophys Res,86(4):2825–2852.

Ekström G,Nettles M,Dziewoński A M. 2012. The global CMT project 2004−2010:Centroid-moment tensors for 13 017 earthquakes[J]. Phys Earth Planet Int,200/201:1–9. doi: 10.1016/j.pepi.2012.04.002

GCMT. 2020. Global CMT catalog[EB/OL]. [2020-06-24]. https://www.globalcmt.org/CMTsearch.html.

Kanamori H,Rivera L. 2008. Source inversion of W phase:Speeding up seismic tsunami warning[J]. Geophys J Int,175(1):222–238. doi: 10.1111/j.1365-246X.2008.03887.x

Wang R J. 1999. A simple orthonormalization method for stable and efficient computation of the Green’s function[J]. Bull Seismol Soc Am,89(3):733–741.

USGS. 2020. M7.4: 13 km ESE of Santa María Xadani, Mexico[EB/OL]. [2020-06-24]. https://earthquake.usgs.gov/earthquakes/eventpage/us6000ah9t/moment-tensor?source=us&code=us_6000ah9t_mww.