
Core-reflected seismic pulse may have nudged Japan after the 2011 megathrust quake
Analysis of Japan’s GNSS data from the 2011 magnitude-9.0 Tōhoku earthquake suggests a seismic wave returning from the core–mantle boundary (ScS) may have triggered a broad, millimeter-to-centimeter fault slip across a large plate boundary, producing tiny but detectable eastward shifts and an energy release comparable to a magnitude 7.5 quake, potentially the first known example of wave-triggered slip from a core-reflected seismic wave; findings published in Science.




