Microseismic monitoring with ocean bottom data is still in its infancy compared to onshore microseismic. A compact PRM system was installed at the Oseberg field in order to monitor a shallow injection well, and in this presentation we have gathered some insights from this project. In addition we compare some properties of the P- and S-wave phases based on modelled microseismic events and we give practical recommendations which will benefit future applications of this technology.


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