TY - GEN
T1 - Drilling into seismogenic zones of M2.0 – M5.5 earthquakes from deep South African gold mines (DSeis)
T2 - ISRM AfriRock 2017 - Rock Mechanics for Africa
AU - the DSeis team
AU - Ogasawara, H.
AU - Durrheim, R. J.
AU - Yabe, Y.
AU - Ito, T.
AU - van Aswegen, G.
AU - Grobbelaar, M.
AU - Funato, A.
AU - Ishida, A.
AU - Ogasawara, H.
AU - Mngadi, S.
AU - Manzi, M. S.D.
AU - Ziegler, M.
AU - Ward, A. K.
AU - Hofmann, G.
AU - Moyer, P.
AU - Boettcher, M.
AU - Dight, P.
AU - Ellsworth, W.
AU - Liebenberg, B.
AU - Wechsler, N.
AU - Onstott, T.
AU - Berset, N.
N1 - Funding Information:
Studies were carried out at six South African gold mines under the auspices of the Japan Science and Technology Agency (JST), the Japan International Cooperation Agency (JICA), and the South African Department of Science and Technology (DST), supplemented by grants from the Japanese Society for the Promotion of Science (JSPS) and other Japanese agencies, the CSIR, and the National Research Foundation, with significant in-kind support from the host gold mining companies (e.g. Ogasawara et al., 2014a). The major project was known as the Science and Technology Research Partnership for Sustainable Development (SATREPS). The main outcomes of the SATREPS project are described in a companion paper (Durrheim et al., 2017).
Publisher Copyright:
© 2017 International Society for Rock Mechanics. All Rights Reserved.
PY - 2017
Y1 - 2017
N2 - While mining-induced earthquakes in the deep gold mines of South Africa pose a risk to mines, mineworkers, and the public, they also provide an unusual opportunity to study the physics of earthquakes. The source zone of a M5.5 earthquake that occurred near Orkney, South Africa on 5 August 2014 was well-defined by tens of thousands of aftershocks recorded by instruments deployed as part of a Japanese - South African research project. The upper edge of the M5.5 rupture is located several hundred metres below the mining horizon. A proposal to drill into the M5.5 source zone, as well as several other active faults in other deep mines, was approved by the International Continental scientific Drilling Programme (ICDP) in August 2016. Here we describe the scope and objectives of the project, and the selection and preparation of the principal drilling sites. In addition to the studies of earthquake phenomena, some of the holes will be used by geomicrobiologists to investigate deep microbiological activity fuelled by hydrogen released by seismic rupture to address questions about early life on planet Earth.
AB - While mining-induced earthquakes in the deep gold mines of South Africa pose a risk to mines, mineworkers, and the public, they also provide an unusual opportunity to study the physics of earthquakes. The source zone of a M5.5 earthquake that occurred near Orkney, South Africa on 5 August 2014 was well-defined by tens of thousands of aftershocks recorded by instruments deployed as part of a Japanese - South African research project. The upper edge of the M5.5 rupture is located several hundred metres below the mining horizon. A proposal to drill into the M5.5 source zone, as well as several other active faults in other deep mines, was approved by the International Continental scientific Drilling Programme (ICDP) in August 2016. Here we describe the scope and objectives of the project, and the selection and preparation of the principal drilling sites. In addition to the studies of earthquake phenomena, some of the holes will be used by geomicrobiologists to investigate deep microbiological activity fuelled by hydrogen released by seismic rupture to address questions about early life on planet Earth.
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M3 - Conference contribution
AN - SCOPUS:85048589628
T3 - ISRM AfriRock - Rock Mechanics for Africa
SP - 237
EP - 248
BT - ISRM AfriRock - Rock Mechanics for Africa
PB - International Society for Rock Mechanics
Y2 - 3 October 2017 through 5 October 2017
ER -