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the relative moment of all events in the sequence. To implement this, we will
separate the matched filter detections out into sequences based first on detecting
template, and then on waveform similarity and hypocentral location. As each template
event
generally represents the largest was detected and processed automatically, a local magnitude
event in has already been assigned to each
of these sequences,
they are likely the best candidate for waveform-based moment tensor inversion. event.
We
propose calculating seismic moment of these template events following the technique
outlined by both Jiao et al. \cite{Jiao_2014} and Guilhem et al. \cite{Guilhem_2014}
and to can use these
moment tensors pre-assigned magnitudes to calibrate the relative moment calculations from the SVD
method. This will work method,
provided each sequence contains only
for sequences which contain at least one template
event for
which event. In this way we
can calculate a reliable moment tensor solution but will
provide be left with accurate
moment local
magnitude
values within these sequences down to potentially very small values.
Using the method of Guilhem and others \cite{Guilhem_2014} to calculate the focal
mechanisms for the templates will allow us to investigate the non-double-couple
components of these events which can account for large percentages of seismic moment
in a geothermal environment \cite{Guilhem_2014}. Furthermore, non-double-couple components of the
moment tensor offer extremely valuable information about the cause of seismicity.
For instance, we might expect to see an increase in the
non-double-couple component of the calculations based on relative moment
tensor near injection wells, transitioning
to largely double-couple events away from calculations via the
well or after well shut-in reflecting
a mechanism which contains parts shear failure and tensile opening in areas where
fluid movement is occurring \cite{Guilhem_2014}. SVD method.
\subsection{Focal Mechanisms}
Calculation of the focal mechanisms for the matched filter-detected events in this study will be done using the approach outlined in \cite{Pugh_2016} which expresses the first motion of a given phase arrival as the probability of both negative and positive polarities instead of the standard, binary "up or down" approach. This approach can also be fully automated which is useful when dealing with datasets of the size of matched filter detection catalogs.