Seismotectonic Architecture and Rupture Dynamics
On , a major megathrust earthquake struck the southern coast of Mindanao, Philippines. The mainshock, which registered a moment magnitude (Mw) of 7.8, occurred within a highly complex convergent boundary zone where the Sunda plate and Philippine Sea plate interact. Seismological agencies recorded varying initial epicentral parameters, illustrating the challenges of real-time monitoring in offshore subduction settings. The United States Geological Survey (USGS) positioned the epicenter at 5.592∘N, 125.047∘E - approximately 26 kilometers west-southwest of Kablalan - with a focal depth of 55.2 kilometers. Conversely, the Philippine Institute of Volcanology and Seismology (PHIVOLCS) initially evaluated the event as a Mw 7.0 crustal earthquake at a depth of 10 kilometers before upgrading it to a tectonic Mw 7.8 rupture at a depth of 33 kilometers, located 32 kilometers south of Maasim, Sarangani.