on
the seismicity concentration in the preceding 19 hours, an approximate N-S fault strike could
have been assumed for the following ML6.5 event, but
considering a longer period, the fault
strike becomes harder to infer from the foreshock distribution.
Following the pattern of historical seismicity, aftershocks of the J-17 earthquake migrated
westwards, with seismicity concentrating in two main
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf