Results 81 to 90 of about 170,936 (206)
A Global Centroid Catalog of S‐Wave Microseisms: Insights Into the Role of Sedimentary Layers
Abstract Although centroid catalogs of P‐wave microseisms have been established, a corresponding centroid catalog of S‐wave sources has been lacking. In this study, we constructed a centroid catalog of S‐wave microseisms. We generalized the autofocusing method to radial and transverse components to estimate the source locations of SV‐ and SH‐wave ...
Shota Kato, Kiwamu Nishida, Ryota Takagi
wiley +1 more source
Harmaline Tremor: Underlying Mechanisms in a Potential Animal Model of Essential Tremor [PDF]
Background: Harmaline and harmine are tremorigenic β-carbolines that, on administration to experimental animals, induce an acute postural and kinetic tremor of axial and truncal musculature.
Handforth, Adrian, Adrian Handforth
core +1 more source
Abrupt Suppression of Tectonic Tremors Outside the Stress Shadow of Mendocino Earthquakes
Tectonic tremor is a long‐duration noise‐like seismic signal associated with slow fault motion at major plate boundaries. Due to their remarkable sensitivity to stress perturbations, tremors serve as invaluable probes of the mechanical state and stress ...
Weifan Lu, Satoshi Ide, Chunmei Ren
doaj +1 more source
The role of velocity‐neutral creep on the modulation of tectonic tremor activity by periodic loading [PDF]
Slow slip events and associated non‐volcanic tremors are sensitive to oscillatory stress perturbations, such as those induced by tides or seismic surface waves. Slow slip events and tremors are thought to occur near the seismic‐aseismic transition regions of active faults, where the differencea − b = ∂μ/∂lnVbetween the sensitivity of friction to slip ...
Ader, Thomas J. +2 more
openaire +2 more sources
Probing Slow Earthquakes With Deep Learning
Slow earthquakes may trigger failure on neighboring locked faults that are stressed sufficiently to break, and slow slip patterns may evolve before a nearby great earthquake.
Bertrand Rouet‐Leduc +3 more
doaj +1 more source
Abstract The 2025 Santorini–Amorgos seismic crisis in Greece had an exceptionally large number and sustained rate of moderate‐sized earthquakes. We used a machine‐learning‐based earthquake monitoring workflow to detect and relocate 66,109 earthquakes and interpret the results in the context of global analogs.
Xing Tan +4 more
wiley +1 more source
Abstract Low‐frequency earthquakes (LFEs) provide key constraints on slow earthquake processes but remain difficult to detect because of their low signal‐to‐noise ratios (SNR) and emergent onsets, particularly in offshore environments where seismic networks are sparse.
Yanhan Chen, Yoshihiro Ito
wiley +1 more source
Tectonic Tremor Explained by Successive Ruptures of Clustered Quartz‐Filled Shear Veins
A tectonic tremor is a successive seismic signal observed along plate boundaries in subduction zones. However, the source processes and mechanisms responsible for the tremor remain unclear. Quartz‐filled shear and extension veins are clustered in tens to
S. Yabe, K. Ujiie
doaj +1 more source
This data manuscript presents a set of signals collected from the Llaima volcano located at the western edge of the Andes in Araucania Region, Chile. The signals were recorded from the LAV station between 2010 and 2016.
João Paulo Canário +4 more
doaj +1 more source
Quantifying the Role of 3D Fault Geometry Complexities on Slow and Fast Earthquakes
Abstract Traditional models of slow slip events (SSEs) oversimplify fault geometry, although imaging shows subduction faults are segmented and complex. We examine how fault interactions control slip behavior using 3D quasi‐dynamic simulations of two parallel faults with uniform rate‐weakening friction accelerated by hierarchical matrices.
J. Cheng +4 more
wiley +1 more source

