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The triggered earthquake of M 3.4 with subsequent events of M >2 was a turning point in the perception of induced seismicity caused by intentional pressure changes in the subsurface. The events followed a massive hydraulic stimulation into granitic basement at 5 km depth below the city of Basel.
The geothermal project attracted worldwide attention, not only because the seismicity was felt throughout the city, but also because, for the first time, induced seismicity was recorded in detail by a scientifically supported monitoring system.
Since then, microseismic monitoring systems have been greatly improved and can now be used in all underground operations where pressure changes occur, such as oil and gas production, fraccing, CCS and EGS.
Place: Ayer’s House, 288 North Tce, Adelaide
The luncheon will consist of 2 courses and drinks
Bookings close 5 pm Friday, 20th June 2025
Any late bookings will incur an additional $20 fee. Strictly no walk-ins.