EGU22-2230, updated on 27 Mar 2022
https://doi.org/10.5194/egusphere-egu22-2230
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Evolution of the DPRK5 and DPRK6 aftershock sequences: 2016 to 2022

Ivan Kitov
Ivan Kitov
  • CTBTO, IDC, WIEN, Austria (ivan.kitov@ctbto.org)

The first aftershock of the announced nuclear test conducted by the DPRK on 09.09.2016 was found by the detection method based on waveform cross correlation on September 11, 2016. This was the only aftershock which was found during the period between the first (09.10.2006) and the sixth (03.09.2017) DPRK tests, using the signals of the DPRK tests as waveform templates. The DPRK6 underground test with mb=6.1 generated a significant aftershock sequence, with some events detected at teleseismic distances. The aftershocks with the best signal quality were used as master events in the multi-master method, working as an active radar focused on the aftershock area. The multi-master method allowed to find more than 100 aftershocks, including 7 aftershocks of the DPRK3 and DPRK4. The aftershock sequence is still active, with 25 aftershocks detected between January 1 and December 10, 2021. The mutual cross correlation of the DPRK aftershocks revealed the presence of two sequences generated by the DPRK5 and DPRK6 cavity collapse. The length, intensity, and alternating character of these two sequences suggest specific mechanisms of energy release. Such a mechanism can be associated with the interaction of the damaged zones of the DPRK5 and DPRK6 and the collapse of their cavities with progressive propagation of the collapsing chimneys towards the free surface. The higher activity in 2021 indicates that the chimney collapse is not finished. We expect more aftershocks, possibly ended with the chimney reaching the free surface.

How to cite: Kitov, I.: Evolution of the DPRK5 and DPRK6 aftershock sequences: 2016 to 2022, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-2230, https://doi.org/10.5194/egusphere-egu22-2230, 2022.