Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

Repeating earthquakes, or repeaters, are identical in location and geometry but occur at
different times. They appear to represent recurring seismic energy release from distinct …

Identification of repeating earthquakes (repeaters) usually depends on waveform similarity
expressed as the corresponding cross‐correlation coefficient (CC) above a prescribed …

Studies of mechanical responses of the Earth crust to large earthquakes can provide us with
unique insights into the processes of stress buildup and release. As a complement to …

We use ambient-noise-based seismic monitoring to detect an anomalous seismic velocity
decrease (∼ 0.01%) widely distributed in Honshu that arose about 1 year after the 2011 M w …

Over the past two decades, the development of the ambient noise cross‐correlation
technology has spawned the exploration of underground structures. In addition, ambient …

In mountainous terrain, large earthquakes often cause widespread coseismic landsliding as
well as hydrological and hydrogeological disturbances. A subsequent transient phase with …

Long‐term and short‐term temporal variations in seismic velocity have been investigated
using seismic interferometry, and significant short‐term changes are typically recognized as …

Abstract Waveform match‐filtering (MF), based on cross‐correlation between an earthquake
pair, is a powerful and widely used tool in seismology. However, its performance can be …

We measured shear wave velocities in the shallow subsurface by applying seismic
interferometry to earthquake records from eight vertical borehole arrays in eastern Hokkaido …