Results 21 to 30 of about 4,644 (163)
Characteristics of Slow Slip Event in March 2020 Revealed From Borehole and DONET Observatories
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 by connecting three borehole stations to the Dense Oceanfloor Network ...
Keisuke Ariyoshi +13 more
doaj +1 more source
Static Source Properties of Slow and Fast Earthquakes [PDF]
AbstractThe source characteristics of slow and fast earthquakes provide a window into the mechanical properties of faults. In particular, the average stress drop controls the evolution of friction, fault slip, and event magnitude. However, this important source property is typically inferred from the analysis of seismic waves and is subject to many ...
Priyamvada Nanjundiah +2 more
openaire +2 more sources
Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution monitoring of slow earthquakes is necessary to understand tectonic conditions.
Satoru Baba +7 more
doaj +1 more source
Tremors are a type of slow earthquake with long‐duration signals compared to ordinary earthquakes. The long signals have been considered to solely reflect their long source process.
A. Toh +3 more
doaj +1 more source
This study investigated the activity and distribution of low-frequency earthquakes (LFEs) accompanying the very low frequency earthquakes (VLFEs) in the central and southern Ryukyu Trench.
Mamoru Nakamura
doaj +1 more source
Subdaily Slow Fault Slip Dynamics Captured by Low‐Frequency Earthquakes
Geodetic positioning is the geophysical record of reference for slow slip events, but typical daily solutions limit studies of the evolution of slow slip to its long‐term dynamics.
Caroline Mouchon +4 more
doaj +1 more source
Laboratory Hydrofractures as Analogs to Tectonic Tremors
The fracture of Earth materials occurs over a wide range of time and length scales. Physical conditions, particularly the stress field and Earth material properties, may condition rupture in a specific fracture regime.
C. Yuan +6 more
doaj +1 more source
Characteristic activities of slow earthquakes in Japan
Slow earthquakes are a recently discovered phenomenon that mainly occur updip and downdip of the seismogenic zones of great earthquakes along the subducting plate interface. The spatiotemporal activity of various slow earthquakes occurring in the Nankai subduction zone is characterized by along-strike heterogeneity and along-dip systematic changes ...
openaire +3 more sources
The High‐Frequency Signature of Slow and Fast Laboratory Earthquakes
AbstractTectonic faults fail through a spectrum of slip modes, ranging from slow aseismic creep to rapid slip during earthquakes. Understanding the seismic radiation emitted during these slip modes is key for advancing earthquake science and earthquake hazard assessment.
Bolton, David C. +6 more
openaire +2 more sources
Shallow Tremors Near the Nankai Trough Activated After the M 7.6 Noto Peninsula Earthquake
Off the Cape Muroto near the Nankai Trough, small shallow tremor activity was observed by distributed acoustic sensing (DAS) and offshore seismic network DONET after the 2024 M7.6 Noto Peninsula earthquake approximately 600 km away.
Satoru Baba, Eiichiro Araki, Takane Hori
doaj +1 more source

