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#Past work  Microseismicity has been observed at Rotokawa since the start of deep injection in 2005 \cite{Sherburn_2015} and at Ngatamariki since injection operations began in 2012 \cite{Sherburn_2013}. At Rotokawa, the largest portion of microseismiciy since 2012 has been located in the southeast portion of the field as discussed in \cite{Sherburn_2015}, within the polygon shown in \ref{Figure 1}.  1. Rotokawa  * Locations normally cluster in the production area within the 'RK04, RK05, RK20' triangle