Results 31 to 40 of about 7,254 (288)
Explaining Slow Earthquake Phenomena with a Frictional-Viscous Faulting Model [PDF]
, 2021 It is well-known that the first-order kinematic characteristics of typical earthquakes, such as slip rate, rupture propagation speed, and moment duration scaling, can be well-explained by a model where the fault experiences a sudden frictional strength ...
Wu, Baoning
core
An intraplate slow earthquake observed by a dense GPS network in Hokkaido, northernmost Japan [PDF]
, 2014 An intraplate slow earthquake was detected in northernmost Hokkaido, Japan, by a dense network of the global navigation satellite system. Transient abnormal acceleration of
Hiroaki Takahashi +5 more
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Earth, Planets and Space, 2017 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
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Subdaily Slow Fault Slip Dynamics Captured by Low‐Frequency Earthquakes
AGU Advances, 2023 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
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Advanced Materials, EarlyView.Drawing inspiration from the layered hard‐soft architecture found in sea sponges, this work establishes a new framework for architected cementitious composites (ACC) through multi‐material additive manufacturing (MMAM) process. The integration of mortar and elastomer phases into layered architectures enables synergistic toughening mechanisms, including
Aimane Najmeddine +5 more
wiley +1 more source
Laboratory Hydrofractures as Analogs to Tectonic Tremors
AGU AdvancesThe 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
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Characteristic activities of slow earthquakes in Japan
Proceedings of the Japan Academy, Series B, 2020 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
Journal of Geophysical Research: Solid Earth, 2022 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
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Daily measurement of slow slip from low-frequency earthquakes is consistent with ordinary earthquake scaling [PDF]
, 2019 Slow slip transients on faults can last from seconds to months and stitch together the earthquake cycle. However, no single geophysical instrument is able to observe the full range of slow slip because of bandwidth limitations.
Frank, William B, Brodsky, Emily E
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Slow slip events and the 2016 Te Araroa Mw 7.1 earthquake interaction: Northern Hikurangi subduction, New Zealand [PDF]
, 2020 Following a sequence of three Slow Slip Events (SSEs) on the northern Hikurangi Margin, between June 2015 and August 2016, a Mw 7.1 earthquake struck ~30 km offshore of the East Cape region in the North Island of New Zealand on the 2 September 2016 (NZ ...
Wallace, L +6 more
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