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In the off-Kamaishi sequence, earthquakes with magnitudes of less than ~3.5 occur multiple times in the slip areas of the M ~ 4.9 mainshocks (Uchida et al., 2007).
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However, in the Kumamoto earthquake sequence, several earthquakes occurred simultaneously within a very narrow range, which was difficult even for the improved system to effectively process.
The same methods, they say, might help create order out of the rapidly accumulating libraries of DNA and protein sequences, earthquake catalogs and other geophysical data.
During the 2016 Kumamoto Earthquake sequence, many crustal earthquakes occurred in the Kumamoto Oita region, central Kyushu, southwestern Japan.
Maybe a sequence of earthquakes discouraged them.
In the existing literature, performance of RC structures under a sequence of earthquakes has received limited attention.
Such a sequence of earthquakes can be regarded as delayed cascade-up.
Displacements, in both horizontal and vertical directions, are naturally increased substantially (w res = 27 cm, δ tot = 45 cm), but the response is judged as satisfactory as the pier remains stable after such a deleterious sequence of earthquakes.
One is the difference between an earthquake sequence and an earthquake swarm, discussed briefly in the last blog entry.
Finally, the probabilistic formulation is illustrated through its application to a building subjected to sequences of earthquakes.
The 2016 Kumamoto earthquake sequence involved several large earthquakes (Shimizu et al. 2016) in the B U area, including along the Futagawa Hinagu fault zone.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com