Results 41 to 50 of about 4,021 (150)
Slow earthquake in Afghanistan detected by InSAR [PDF]
The Chaman fault system forms a prominent ∼900‐km‐long left‐lateral transform plate boundary between the Indian and Eurasian plates in Afghanistan and Pakistan. Here we show satellite radar interferometry data that revealed an afterslip (or slow earthquake) signal following an earthquake of magnitude 5.0.
Furuya, M., Satyabala, S. P.
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Slow slip events are regular earthquakes [PDF]
Abstract Slow slip events usually occur downdip of seismogenic zones in subduction megathrusts and crustal faults, with rupture speeds much slower than earthquakes. The empirical moment-duration scaling relation can help constrain the physical mechanism of slow slip events, yet it is still debated whether this scaling is linear or cubic and a ...
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Deep long period volcanic earthquakes generated by degassing of volatile-rich basaltic magmas
The origin of deep long-period earthquakes beneath active volcanoes that are sometimes considered as precursors to eruptions remains not fully understood. Here the authors show that these earthquakes can be generated by the rapid degassing in response to
Oleg Melnik +4 more
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Slow Stick‐Slip Failure in Halite Gouge Caused by Brittle‐Plastic Fault Heterogeneity
Slow earthquakes, including low‐frequency earthquakes and tremor, occur in the brittle‐ductile (plastic) transition zone on plate boundary faults. To understand how transitions in deformation mechanisms can influence seismic behavior, we conducted stick ...
Ken‐ichi Hirauchi +3 more
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We examined the possible factors affecting the spatial distribution of very low frequency earthquakes and tremors in the shallow megathrust of Nankai Trough (
Paul Caesar M. Flores +7 more
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Co‐Occurrence of Low and Very Low Frequency Earthquakes Explained From Dynamic Modeling
Very low‐frequency earthquakes (VLFs) are characterized by longer source duration and smaller stress drop than regular earthquakes of similar magnitude. Recent studies have shown their frequent correlation with low‐frequency earthquakes (LFEs) on shared ...
Xueting Wei +3 more
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Landslides accompanying earthquakes are essential in landscape evolution along active fault zones. However, most studies focus on the rapid, catastrophic coseismic landslides with surface scars; the role of slow-moving landslides and their relation with ...
Lv Fu, Teng Wang
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High time-resolved studies of stick-slip show similar dilatancy to fast and slow earthquakes. [PDF]
Hu W +10 more
europepmc +1 more source
Unraveling the Origin of Slow Earthquakes
Different nucleation styles detected in five slow-slip events in the same area of Japan’s Ryukyu subduction zone suggest the physical properties along this tectonic plate interface change over time.
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Upper-plate conduits linked to plate boundary that hosts slow earthquakes. [PDF]
Arai R +11 more
europepmc +1 more source

