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 …

Repeating earthquakes (repeaters) that rupture the same fault area (patch) are interpreted to
be caused by repeated accumulation and release of stress on the seismic patch in a …

We carry out high‐resolution three‐dimensional seismic tomography of the crust and upper
mantle beneath southwestern (SW) Japan using arrival‐time data obtained from the …

We first determine the configuration of the upper surface of the Pacific (PAC) slab beneath
Kanto, Japan, from the distribution of interplate earthquakes relocated by an appropriate 1 …

Non-volcanic deep low-frequency tremors in southwest Japan exhibit a strong temporal and
spatial correlation with slow slip detected by the dense seismic network. The tremor signal is …

Fluid migration and pore fluid pressure have been implicated in generating the transitional
fault zone properties thought to be important for slow slip events (SSEs) in subduction …

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

Interplate coupling in the southernmost extent of the northeast Japan subduction zone (east
off-Kanto, Japan) is investigated in detail using a large data set of small repeating …

ABSTRACT The 1923 Taisho Kanto earthquake—an interplate event along the Sagami
trough where the Philippine Sea plate subducts beneath the Kanto region—produced …

Abstract Knowledge of what governs the timing of earthquakes is essential to understanding
the nature of the earthquake cycle and to determining earthquake hazard, yet the variability …