Improvements in magnitude precision, using the statistics of relative amplitudes measured by cross correlation

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Fluid‐faulting evolution in high definition: Connecting fault structure and frequency‐magnitude variations during the 2014 Long Valley Caldera, California, earthquake swarm (2016, methodology): “The principal component fit (red line) preserves the reciprocal relationship, but the least squares solution (black dashed line) is biased, showing lower apparent amplitude of the detected event, due to imperfect correlation [Schaff and Richards, 2014].”