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The Reykjafjall N–S source fault ruptured during the M w 6.3 earthquake doublet on May 29, 2008, in the South Iceland Seismic Zone (SISZ). The northern part of the fault intersects the easternmost high-temperature geothermal field of Hengill in an extinct volcano that began shifting away from the Western Rift Zone 120,000 years ago. Geophysical data indicate that the N–S fault ruptured over...
In this paper we present a review of controlling geological, tectonic and engineering factors for induced seismicity associated to gas depletion in the Netherlands and we place experiences from extensive Dutch geomechanical studies in the past decade in the context of generic models for induced seismicity. Netherlands is in a mature gas production phase, marked by excellent subsurface structural and...
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