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Fault creep on the central segment of the Longitudinal Valley fault, Eastern Taiwan. Holocene tectonic uplift on the Hua-Tung coast, Eastern Taiwan. Vertical crustal movement in eastern Taiwan and its tectonic implications. Stratigraphic record of plate interactions in the Coastal Range of Eastern Taiwan. An Introduction to the Geology of Taiwan: Explanatory Text of the Geologic Map of Taiwan 2nd edn (Central Geological Survey, Taiwan, 1986)Ĭhi, W. Kinematics of arc-continent collision, flipping of subduction, and back-arc spreading near Taiwan. Detection of triggered deep low-frequency events from the 2003 Tokachi-oki earthquake. Periodically triggered seismicity at Mount Wrangell, Alaska, after the Sumatra earthquake.
Earthquake nucleation by transient deformations caused by the M = 7.9 Denali, Alaska, earthquake. A new observation of dynamically triggered regional seismicity: earthquakes in Greece following the August, 1999 Izmut, Turkey earthquake. Seismicity remotely triggered by the magnitude 7.3 Landers, California, earthquake. Consequences of stress changes following the 1891 Nobi earthquake, Japan. Asthenospheric viscosity inferred from correlated land–sea earthquakes in north-east Japan. A possible model for large preseismic slip on a deeper extension of a seismic rupture plane. Slow earthquakes and great earthquakes along the Nankai trough. Slow earthquakes coincident with episodic tremors and slow slip events. Ito, Y., Obara, K., Shiomi, K., Sekine, S. Geodetic and seismic signatures of episodic tremor and slip in the northern Cascadia subduction zone. Constraints on slow earthquake dynamics from a swarm in central Italy. Silent fault slip following an interplate thrust earthquake at the Japan Trench. A slow earthquake sequence on the San Andreas fault.
Measurements of the strain field associated with episodic creep events on the San Andreas fault at San Juan Bautista, California. Stress redistribution and slow earthquakes. Slow earthquakes and stress redistribution. This area experiences very high compressional deformation but has a paucity of large earthquakes repeating slow events may be segmenting the stressed area and thus inhibiting large earthquakes, which require a long, continuous seismic rupture. Lower pressure results in a very small unclamping of the fault that must be close to the failure condition for the typhoon to act as a trigger.
We model the largest of these earthquakes as repeated episodes of slow slip on a reverse fault just under land and dipping to the west the characteristics of all events are sufficiently similar that they can be modelled with minor variations of the model parameters. Here we show that, in eastern Taiwan, slow earthquakes can be triggered by typhoons. Triggering of earthquakes has received much attention: strain diffusion from large regional earthquakes has been shown to influence large earthquake activity 11, 12, and earthquakes may be triggered during the passage of teleseismic waves 13, a phenomenon now recognized as being common 14, 15, 16, 17. It has been suggested 9 that the slow events may trigger ordinary earthquakes (in a context supported by numerical modelling 10), but their broader significance in terms of earthquake occurrence remains unclear. Since then, many slow earthquakes have been detected 3, 4, 5, 6, 7, 8. The first reports 1, 2 on a slow earthquake were for an event in the Izu peninsula, Japan, on an intraplate, seismically active fault.