1887

Abstract

Passive seismic monitoring has been ongoing at the IEA GHG Weyburn-Midale Project since 2003. We present the microseismic activity recorded during a 5 year period, showing event timings and locations, and discussing the implications for storage integrity. We link passive seismic observations with predictions about event locations and seismic anisotropy made by a simple geomechanical model, demonstrating the importance of combining observation with modelling in order to guarantee successful storage.

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/content/papers/10.3997/2214-4609.201400923
2010-06-14
2020-09-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400923
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