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- W4384202274 abstract "Abstract Tremor signals are weak and emergent, and the physics governing their generation is not well understood. Here, I report on tremor occurring along the Dead Sea Transform (DST), and a microearthquake on the Carmel-Fari'a Fault (CFF), both dynamically triggered by the 2023 M w 7.6 Kahramanmaraş earthquake. The triggered events location coincides with maxima of long-period velocity gradients, concentrated in the CFF-DST intersection and near a CFF fault-jump. Relative to other remotely triggered tremors, the DST tremor is strong and deficient in high-frequency seismic energy. Furthermore, analysis of several triggered tremor episodes suggests that tremors spectral fall-off rates are not universal. I discuss the seismological attributes that may give rise to these observations in the context of two models. In the first, tremor is produced due to inertial vibrations of a frictionally-controlled oscillator, and in the second it is produced by a swarm of Low-Frequency Earthquakes." @default.
- W4384202274 created "2023-07-14" @default.
- W4384202274 creator A5018926854 @default.
- W4384202274 date "2023-07-13" @default.
- W4384202274 modified "2023-09-30" @default.
- W4384202274 title "Dynamic triggering along the Dead Sea transform uncovers tremor source physics" @default.
- W4384202274 doi "https://doi.org/10.21203/rs.3.rs-3067902/v1" @default.
- W4384202274 hasPublicationYear "2023" @default.
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