The great March 25, 1998, Antarctic Plate earthquake: Moment tensor and rupture history

We use broadband body and mantle wave data to study the 1998 Antarctic intraplate earthquake. The centroid moment tensor (CMT) has a large non-double-couple component. There exist two pure double-couple constrained solutions that fit the data almost equally well. The frequent practice of taking the "best double-couple" gives a far from optimal solution. We use P and SH body waves to determine the rupture parameters of the first and larger of the two observed subevents. The best rupture plane, with strike 96°, dip 69°, and rake -18°, is compatible with only one of the two CMT solutions: strike 96°, dip 64°, rake -23°, centroid location (63.1°S, 148.4°E, 10 km depth), centroid time 0313:02 UT, and M₀ = 1.3 × 10²¹ N m (M_w = 8.0). The first subevent is a simple, primarily westward propagating ∼140-km rupture, of ∼45-s duration, with average velocity ≳3 km s^-1; it has a seismic moment of 1.2×10²¹ N m (M_w = 8.0), with 75% of its moment released between 10 and 27 s, and a stress drop of ∼240 bars. The rupture is physically bounded by two fracture zones at 147.5°E and 150°E. The second subevent lasted from 70 to 90 s on a fault extending from 210 to 270 km west of the epicenter, with a moment of 0.3-0.6×10²¹ N m (M_w = 7.6-7.8). This is a spectacular example of dynamic stress triggering over a 100-km separation distance with a time delay of ∼40 s. The complex pattern of aftershocks is primarily controlled by preexisting fracture zones on the ocean floor.