Preprints
https://doi.org/10.5194/se-2020-58
https://doi.org/10.5194/se-2020-58

  12 May 2020

12 May 2020

Review status: this preprint was under review for the journal SE. A final paper is not foreseen.

Statistics of the Seismic Sequence and Rupture Directivity of the M5.5 Earthquake in Orkney, South Africa

Carsten Dinske1, Jonas Folesky1, Jörn Kummerow1, Serge Shapiro1, and Hiroshi Ogasawara2 Carsten Dinske et al.
  • 1Freie Universität Berlin, Department of Earth Sciences, Geophysics, Berlin, Germany
  • 2Ritsumeikan University, College of Science and Engineering, Kusatsu, Japan

Abstract. Despite our general knowledge of earthquake processes, it is still not fully understood how earthquake ruptures nucleate and propagate and why they stop. Also, the controlling factors of the frequency and of the size of earthquakes are subject of ongoing research. We aim to address these questions with a comprehensive study of seismicity in deep South African gold mines. We find here the unique situation that the seismicity consists of both induced earthquakes and aftershocks triggered by the M5.5 Orkney earthquake which occurred in August 2014. We separate the cataloged seismicity and group the events into three classes: the aftershock sequence, seismicity induced by fluids, and seismicity induced by mining activities. We examine statistical properties of earthquakes in each of the three classes. We conclude that the magnitude statistics of both aftershocks and induced earthquakes are influenced by the finite size and geometry of the rock volume of stress perturbation resulting in an absence of larger magnitude events. The magnitude frequency distributions obey the Lower Bound model of magnitude probability. The statistics of dynamic stress drop of aftershocks and induced earthquakes satisfy log-normal distributions but the value range is different, it means that aftershocks are generally characterized by higher stress drops. Another key aspect in our study is the imaging of the propagating rupture of the M5.5 earthquake. We apply the back projection imaging approach using seismological data from two different local networks and retrieve similar results. We conclude that the rupture of the M5.5 earthquake propagated predominantly unilaterally, nearly from North to South over a distance of about 6km. The hypocenters of the aftershock sequence are situated unilaterally in respect to the hypocenter of the main shock and are aligned to the South which confirms the obtained rupture propagation image and the directivity of the main shock.

This preprint has been withdrawn.

Carsten Dinske et al.

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Carsten Dinske et al.

Carsten Dinske et al.

Viewed

Total article views: 440 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
246 138 56 440 50 42
  • HTML: 246
  • PDF: 138
  • XML: 56
  • Total: 440
  • BibTeX: 50
  • EndNote: 42
Views and downloads (calculated since 12 May 2020)
Cumulative views and downloads (calculated since 12 May 2020)

Viewed (geographical distribution)

Total article views: 335 (including HTML, PDF, and XML) Thereof 335 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 23 Sep 2021
Download

This preprint has been withdrawn.

Short summary
We analyse seismicity in deep South African gold mines. We find here the unique situation that it consists of both induced earthquakes and aftershocks triggered by the M5.5 Orkney earthquake. We conclude that the magnitude statistics of aftershocks and induced earthquakes are influenced by the size and geometry of the volume of stress perturbation. We also image the propagating rupture of the M5.5 earthquake. We conclude that it propagated unilaterally from North to South over a distance of 6km.