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\section{Results \chapter{Preliminary results  and discussion} \section{Objective 1}  \subsection{Matched Filter detections}  Using all 637 template events, we were able to detect more than 20,000 additional events from 1 January to 20 November, 2015. A large majority of these (>12,000) were located in Rotokawa while slightly less than 4000 events were located in Ngatamariki (Figure \ref{Figure2}). These numbers conform to the 3:1 Rotokawa-Ngatamariki seismicity ratio mentioned earlier (e.g. \cite{Sherburn&Bourguignon_2015}, \cite{Sherburn&Johnson_2015}). Detections have been clustered into three basic groups: Rotokawa, northern Ngatamariki and southern Ngatamariki, based upon historic seismicity. The cumulative detections for each of these groups is plotted with time for the study period along with pumping rates for pertinent injection wells (Figs. \ref{Figure3}, \ref{Figure4}, \ref{Figure5}).