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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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Imaging evolution of Cascadia slow-slip event using high-rate GPS. [PDF]
Itoh Y, Aoki Y, Fukuda J.
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Tectonic tremors could offer insights into the big shakers [PDF]
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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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Volcanic crisis reveals coupled magma system at Santorini and Kolumbo. [PDF]
Isken MP +32 more
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A strength inversion origin for non-volcanic tremor. [PDF]
Vannucchi P +5 more
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Insights into the seismogenesis and tectonic implications of an isolated intraplate earthquake (M4.0) on February 17, 2025, in Delhi. [PDF]
Prajapati SK +4 more
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Tiny stresses are capable of triggering earthquakes and tremors in Arunachal Himalaya. [PDF]
Saini T +4 more
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