Deep tectonic tremor has been observed in a number of plate-bounding tectonic environments around the world. It can occur both spontaneously (i.e. ambient) and as a result of small stress perturbations from passing seismic waves (i.e. triggered). Because
Zimmerman, Jessica P. +2 more
core
Structural barriers control the spatial extent of slow earthquake slip. [PDF]
Akuhara T +18 more
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Active protothrusts and fluid highways: Seismic noise reveals hidden subduction dynamics in Cascadia. [PDF]
Kidiwela M +3 more
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Fault-mediated magma propagation and triggered seismicity revealed by the 2022 São Jorge Azores unrest. [PDF]
Hicks SP +21 more
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Hidden patterns in volcanic seismicity: deep learning insights from Mt. Etna's 2020-2021 activity. [PDF]
Abed W +9 more
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Seismological Structures on Bimodal Distribution of Deep Tectonic Tremor
Deep tectonic tremors occur at the downdip extent of the seismogenic zone due to fluid processes. Beneath the northeastern Kii Peninsula, southwestern Japan, there is an along-dip bimodal distribution of tremor. However, no constraint exists on the structures controlling that distribution.
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How earthquakes organize stress. [PDF]
Brodsky EE, Farge G.
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Slow slip modulates low-frequency seismicity on the Parkfield segment of the San Andreas Fault. [PDF]
Zali Z +3 more
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Secondary acceleration of slip fronts driven by slow slip event coalescence in subduction zones. [PDF]
Wang J +7 more
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Imaging evolution of Cascadia slow-slip event using high-rate GPS. [PDF]
Itoh Y, Aoki Y, Fukuda J.
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