[M-IS02] 地球掘削科学

[MIS02-10] ICDP DSeis 3: Spatial variation in stress state in the source region of Orkeny earthqauke (M5.5) based on analyses of the ICDP-DSeis borehole cores

*矢部 康男¹、石田 亮壮²、杉村 幸祐²、兼松 慎²、東 充也²、吉田 峻輔²、Liebenberg Bennie⁷、伊藤 高敏³、船戸 明雄⁵、Watson Bryan⁶、Durrheim Raymond⁴、小笠原 宏² (1.東北大学大学院理学研究科附属地震・噴火予知研究観測センター、2.立命館大学理工学部、3.東北大学流体科学研究所、4.School of Geoscience, University of the Witwatersrand、5.深田地質研究所、6.School of Mining Engeneering, University of the Witwatersrand、7.Moab Khotsong mine)

キーワード：ICDP-DSeis、応力測定、変形率変化法、コア変形法、南アフリカ大深度金鉱山

The Orkney earthquake (M5.5), South Africa, occurred on 5 August 2014 beneath a deep gold mine, of which the deepest mining horizon is ~3 km depth from ground surface. Hypocenter of the Orkney earthquake and the shallowest aftershocks were located at ~5 km and ~3.5 km depths from ground surface. Therefore, the ICDP-DSeis project was devised to investigate the geological, geomechanical and geochemical environments in and around the source region of the Orkney earthquake. Two 800 m-long boreholes (Holes A and B) were drilled from a drilling site established on a tunnel at a depth of 2.8 km in the mine. While Hole A reached the seismogenic depth, it did not intersect the aftershock cluster. Hole B success fully penetrated to the aftershock cluster. Borehole cores were almost fully recovered from these holes, though they were not oriented during drilling. Therefore, the core orientation was determined by comparing in-hole optical images and unrolled core images in this study. Then, Diametrical Core Deformation Analysis (DCDA, Funato and Ito, 2017) and Deformation Rate Analysis (DRA, Yamamoto et al., 1990) were applied to borehole cores to evaluate a spatial variation in stress state in and around the aftershock cluster. Finally, a numerical elastic model in which the depth variations along Hole A and B were reproduced was developed to understand a spatial distribution of stress state in and around the aftershock cluster that extended along upper extension of the source fault of the Orkney earthquake.



Acknowledgement. This study was supported by ICDP, JSPS-NRF bilateral research project, JSPS Core-to-Core program, Ritsumeikan University and the Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan, under its Earthquake and Volcano Hazards Observation and Research Program. The authors thank Harmony Gold Ltd. for kindly providing an opportunity of drilling from Moab Khotsong mine.