that a tectonic earthquake like the 1912 earthquake in the eastern South Icelandic Seismic
Zone or 1963 in Skagafjörður (both were around magnitude 7) can easily outnumber the recent activity
around Bárðarbunga in just one event, by means of moment release.
The cumulative moment release during the migration of the dyke intrusion between 16 August and 1
September corresponds to a single
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