2019 status report: Drilling into seismogenic zones of M2.0–M5.5 earthquakes in South African gold mines (DSeis project)

H. Ogasawara, B. Liebenberg, M. Rickenbacher, M. Ziegler, H. V. Esterhuizen, T. Onstott, R. Durrheim, M. Manzi, S. Mngadi, Y. Yabe, S. Kaneki, E. Cason, Jan-G. Vermeuren, E. Heerden, T. Wiersberg, M. Zimmer, C. Kujawa, R. Conze, G. V. Aswegen, N. Wechsler, A. Ward, S. Enslin, S. Tau, Mavuso Bucibo, DSeis Team
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引用次数: 1

Abstract

In 2014, a M5.5 earthquake ruptured the range of depths between 3.5 km and 7 km near Orkney, South Africa. The main and aftershocks were very well monitored in the nearfield by dense, surface, strong motion meters and a dense underground seismic network in the deep gold mines. The mechanism of this M5.5 earthquake was left-lateral strike-slip faulting, differing from typical mining-induced earthquakes with normal-faulting mechanisms on the mining horizons shallower than 3.5 km depth. To understand why such an unusual event took place, the aftershock zone was probed by full-core NQ drilling during 2017-2018, with a total length of about 1.6 km, followed by in-hole geophysical logging, core logging, core testing, and monitoring in the drilled holes. These holes also presented a rare opportunity to investigate deep life. In addition, seismogenic zones of M2–M3 earthquakes were probed on mine horizons that were also very well monitored by acoustic emission networks. This paper reviews the early results of the project.
2019年现状报告:南非金矿2.0 - 5.5级地震发震带钻探(DSeis项目)
2014年,南非奥克尼附近发生了5.5级地震,震源深度在3.5公里到7公里之间。通过密集的地表强震仪和密集的地下地震台网,在近场对主震和余震进行了很好的监测。此次5.5级地震的发生机制为左旋走滑断裂,不同于3.5 km以下采动层的典型采动地震的正常断裂机制。为了解这一异常事件发生的原因,在2017-2018年期间,采用全岩心NQ钻井对余震区进行了探测,总长度约为1.6 km,随后进行了井内地球物理测井、岩心测井、岩心测试和钻孔监测。这些洞也为研究深层生命提供了难得的机会。此外,还在矿区层位探测了M2-M3地震发震带,声发射网对这些发震带进行了很好的监测。本文回顾了该项目的早期成果。
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