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Figure 4, panel A shows the topographic map of event origins: 54% of events originated in the frontal area, 15% in the central, 17% in the temporal and 14% in the posterior.
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The event origin location, i.e. the location from which the propagating SSO originates was detected searching for the channel containing the first occurring negative peak.
However, more work is needed to confirm or exclude an extraterrestrial impact event origin and to determine if microspherules and/or Pt-rich dust are the carriers of Pt and other PGEs in the YDB layer.
The results show that, when a dense seismic network is deployed in the fault area, PRESTo can produce reliable estimates of earthquake location and size within 5 6 s from the event origin.
Time since the event origin is shown.
Fig. 9. Variation of displacement magnitudes versus elapsed time from the event origin time.
Valuable results for tsunami warning purposes were obtained 20 min after the event origin time.
The horizontal axis denotes the elapsed time from the event origin time.
Mwp at stations become stable after about four minutes from the event origin time.
The elapsed time from the event origin time (01 25 05 on April 16, 2016 JST) is also shown.
Acoustic bearings and event origin times inferred from array processing are consistent with the eyewitness accounts.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com