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Nature 424, 921-925 (21 August 2003) | doi:10.1038/nature01903;
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Remote triggering of deep earthquakes in the 2002 Tonga sequences
It is well established that an earthquake in the Earth's crust can trigger subsequent earthquakes, but such triggering has not been documented for deeper earthquakes. Models for shallow fault interactions suggest that static (permanent) stress changes can trigger nearby earthquakes, within a few fault lengths from the causative earthquake, whereas dynamic (transient) stresses carried by seismic waves may trigger earthquakes both nearby and at remote distances.
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