Gravity-induced seismicity modulation on planetary bodies and their natural satellites. [PDF]
Senapati B, Kundu B, Jha B, Jin S.
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Stress heterogeneities in exhumed high-pressure rocks shed light on deep subduction interface transient coupling. [PDF]
Wu Y +5 more
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Burst-like swarms in the Campi Flegrei caldera accelerating unrest from 2021 to 2024. [PDF]
Giudicepietro F +26 more
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Tidal and hydrological seismicity modulations reveal pore fluid diffusion during earthquake nucleation. [PDF]
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Ambient noise levels of seismic stations located in urban agglomerations in central Inner Mongolia, China. [PDF]
Bao W, An Q, Guo Y, Wang L, Gao J.
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Subduction intraslab-interface fault interactions in the 2022 Mw 6.4 Ferndale, California, earthquake sequence. [PDF]
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Tidal sensitivity of tectonic tremors and frictionally heterogeneous fault model
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Continental Crust Anisotropy Measurements From Tectonic Tremor in Cascadia
Journal of Geophysical Research: Solid Earth, 2017AbstractWe present new observations of crustal anisotropy in the southern Cascadia fore arc from tectonic tremor. The abundance of tremor activity in Oregon and northern California during slow‐slip events offers an enormous amount of information with which to measure and analyze anisotropy in the upper brittle continental crust.
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A Glimpse Into the Future of Tectonic Tremor Monitoring
Journal of Geophysical Research: Solid EarthAbstract Tectonic tremor is a weak, long‐duration seismic signal often observed in subduction zones and on some other plate‐bounding faults. Because of tremor's characteristically low amplitude (and low signal‐to‐noise) and lack of clear phase arrivals, detecting and locating tremor usually requires techniques ...
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Cataloging Tectonic Tremor Energy Radiation in the Cascadia Subduction Zone
Journal of Geophysical Research: Solid Earth, 2021Abstract For the past ∼12 years the Pacific Northwest Seismic Network has been automatically detecting and locating tectonic tremor across the Cascadia subduction zone, resulting in a catalog of more than 500,000 tremor epicenters to date, which has served as a valuable resource for tremor and slip research.
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