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Australia: The Land Where Time Began |
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Most Large Interplate Earthquakes Have a Long Precursory Phase According to the authors1 many earthquakes are preceded by foreshocks (Jones & Molnar, 1976; Jones & Molnar, 1979). The reason they occur before some earthquakes and not others, and the mechanisms generating the foreshocks, is unknown (3,8). In this study the authors1 used seismic catalogues from the best instrumented areas of the North Pacific and analysed the foreshock sequences that preceded all earthquakes that occurred 1999-2011, with a magnitude greater than 6.5 and shallower than 50 km. They used a dataset comprising 31 interplate, occurring at plate boundaries, earthquakes and 31 intraplate, earthquakes occurring within the same plate. The authors1 found a much strong correlation between foreshock sequences and interplate quakes than between foreshock sequences and intraplate quakes. In the North Pacific most large interplate earthquakes were preceded by accelerating seismic activity over the months to days leading up to the main shock, though foreshocks are much less common before intraplate earthquakes. The authors1 suggest that the interface between plate boundaries begins slipping slowly before the rupture that results in a large earthquake. They also suggest that in the case of interplate earthquakes the precursory phase, that is relatively long, could help mitigate risk associated with interplate earthquakes.
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |