Abstract National Research Institute for Earth Science and Disaster Resilience (NIED)
integrated the land observation networks established since the 1995 Kobe earthquake with …

The Moho in subduction zones exists in two distinct forms, one associated with the
subducting oceanic plate and second with the overriding plate. The seismic expression of …

Non-volcanic tremor and related slow earthquakes in subduction zones are one of the most
significant and exciting geophysical discoveries of the 21st century. In Japan, some types of …

The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

The phenomenology of deep slow earthquakes, including low‐frequency tremors, very low
frequency earthquakes, and short‐term slow slip events, on the subducting plate interface in …

We construct fine-scale 3D P-and S-wave velocity structures of the crust and upper mantle
beneath the whole Japan Islands with a unified resolution, where the Pacific (PAC) and …

With a new location method, we obtained a high‐resolution map of non‐volcanic tremor
along the subducting Philippine Sea plate in southwest Japan and clarified the depth …

The spatiotemporal patterns of the radiated seismic energy from low‐frequency tremor
associated with slow slip events in western Shikoku, Japan, have been estimated. A …

In southwestern Japan, the Philippine Sea plate subducts beneath the Eurasian plate. Non-
volcanic tremors and slow slow-slip events are observed beneath southwestern Japan …

Short‐term slow slip events accompanied by nonvolcanic deep low‐frequency tremors and
deep very low frequency earthquakes in southwest Japan were investigated systematically …