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

The discovery of slow earthquakes has revolutionized the field of earthquake seismology.
Defining the locations of these events and the conditions that favor their occurrence provides …

Marine geohazard research has developed during recent decades, as human activities
intensified towards deeper waters. Some recent disastrous events (eg, the 2004 Indian …

Abstract In 2014–2015, the Hikurangi Ocean Bottom Investigation of Tremor and Slow Slip
experiment deployed seafloor absolute pressure gauges and ocean bottom seismometers …

A low-velocity zone (LVZ) has been detected by seismic exploration surveys within the
Nankai accretionary prism toe off the Kii Peninsula, southwestern Japan, and is considered …

We have detected an event of pore pressure change (hereafter, we refer it to “pore pressure
event”) from borehole stations in real time in March 2020, owing to the network developed …

This paper is devoted to the features of seismological observations in the Arctic seas, which
are complicated by harsh climatic conditions, the presence of ice cover, stamukhi and …

The Nankai subduction zone off the Kii Peninsula, Japan, has a large potential to generate
megathrust earthquakes in the near future. To investigate the temporal variation of stress or …

Deep and shallow slow earthquakes occur at the edge of the seismogenic zone in the
Nankai subduction zone. Deep slow earthquakes occur under high‐temperature and high …

Geodetic observations in the oceans are important for understanding plate tectonics,
earthquake cycles and volcanic processes. One approach to seafloor geodesy is the use of …