Japan Geoscience Union Meeting 2016

Presentation information


Symbol S (Solid Earth Sciences) » S-SS Seismology

[S-SS27] Fault Rheology and Earthquake Physics

Thu. May 26, 2016 10:45 AM - 12:10 PM Convention Hall A (2F)

Convener:*Takeshi Iinuma(National Research and Development Agency Japan Agency for Marine-Earth Science and Technology), Yuko Kase(Geological Survey of Japan, AIST), Ryosuke Ando(Graduate School of Science, University of Tokyo), Wataru Tanikawa(Japan Agency for Marine-Earth Science and Technology, Kochi Instutute for Core Sample Research), Hideki Mukoyoshi(Department of Geoscience Interdisciplinary Graduate School of Science and Engineering, Shimane University), Chair:Kazutoshi Imanishi(National Institute of Advanced Industrial Science and Technology), Ayumi S. Okamoto(Department of Natural History Sciences, Graduate School of Science, Hokkaido University)

11:25 AM - 11:40 AM

[SSS27-17] Aftershock distribution and focal mechanisms of 2014 Mw5.4 Orkney earthquake, South Africa, by using underground seismic networks in gold mines

*Kazutoshi Imanishi1, Hiroshi Ogasawara2, Yasuo Yabe3, Shigeki Horiuchi4, Makoto OKUBO5, Osamu Murakami6 (1.Geological Survey of Japan, AIST, 2.Faculty of Science and Engineering, Ritsumeikan University, 3.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, 4.Home Seismometer Corporation, 5.National Science Cluster, Kochi University, 6.Tono Research Institute of Earthquake Science, Association for the Development of Earthquake Prediction)

Keywords:2014 Mw5.4 Orkney earthquake , Gold mines, South africa, Aftershock distribution, Focal mechanism

The Mw5.4 Orkney earthquake occurred on August 5, 2014, near Orkney town, South Africa. The mainshock and aftershocks were recorded by underground networks in gold mines, which are composed of 46 three-component geophones installed at 2-3 km depths. The sampling rate is 6 kHz. The observed waveforms have high signal-to-noise ratios and contain higher frequency components up to at least 1 kHz, which provide the opportunity for precise determination of aftershock distribution and source parameters. We determined hypocenters of 2000+ aftershocks by automatic earthquake location software from Home Seismometer Corp. (Horiuchi et al., 2011). Aftershocks distributed at depths from about 4 to 7 km forming a 8 km-long in the NNW-SSE direction. The distribution agrees with one of nodal planes of the mainshock focal mechanism, suggesting that the mainshock represents a left lateral strike-slip fault. Aftershock focal mechanisms were determined from P-wave polarity data as well as body wave amplitudes. As a preliminary analysis, we analyzed aftershocks with at least 15 P-wave polarities and obtained 137 well-determined solutions. Most of aftershocks show a pure strike-slip mechanism that is similar to the mainshock. We also found some aftershocks whose P- and T- axis deviates from the general trend and contain normal or reverse faulting components. These events seem to distribute at the middle and the north of the aftershock distribution, suggesting the existence of local stress heterogeneity. Further analysis of aftershocks is needed to elucidate whether the heterogeneity was caused by stress changes due to the mainshock and/or associated with locally formed pre-mainshock stress regime.
Acknowledgements. The seismic network used in this study is operated by Anglogold Ashanti and Open House Management Solutions. The data processing was performed by Institute of Mine Seismology. The data ownership belongs to Anglogold Ashanti.