JpGU-AGU Joint Meeting 2020

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-SS Seismology

[S-SS15] Fault Rheology and Earthquake Physics

convener:Keisuke Yoshida(Tohoku University), Keishi Okazaki(Japan Agency for Marine-Earth Science and Technology), Shunya Kaneki(Disaster Prevention Research Institute, Kyoto University), Hiroyuki Noda(Kyoto University, Disaster Prevention Research Institute)

[SSS15-02] ICDP DSeis: Mineralogical, chemical, and frictional characteristics of fault-related rocks recovered from the Moab Khotsong gold mines in South Africa

Yuki Yokoyama1, *Tetsuro Hirono1, Hiroshi Ogasawara2, Tsuyoshi Ishikawa3 (1.Department of Earth and Space Science, Graduate School of Science, Osaka University, 2.Ritsumeikan University, 3.Kochi Institute for Core Sample Research, JAMSTEC)

Keywords:Deep drilling of fault

Drilling into the rupture zone of M5.5 Orkney earthquake was conducted at the Moab Khotsong gold mine at 2.9 km depth, and core samples, including fault-related rocks, were successfully collected. The samples are divided into the Roodepoort formation, the Crown formation and the Babrosco formation, and the fault zone developed in ignious intrusion within the Crown lava. By performing mineralogical and chemical analyses and microscopic observation, the main fault is mainly composed of talc, biotite, amphibole (tremolite), and calcite, whereas the host rocks contains quartz, feldspar, and chlorite. Shear foliation is microscopically observed in the fault. The frictional coefficient of the fault is 0.54 whereas those of surrpunding host rocks are 0.68 – 0.75.

The intrusion and main fault are intensively altered, but the original rock type of the intrusion is estimated to be Lamprophyre on the basis of the mineral and chemical compositions, thus indicating that seismic deformation is concentrated in the lamprophyre with high amoung of talc and low frictional coefficient.