Abstract

Accurate identification and picking of P- and S-wave arrivals is important in earthquake and exploration seismology. Often, existing algorithms are lacking in automation, multiphase classification and picking, as well as performance accuracy. We have developed a new fully automated four-step workflow for efficient classification and picking of P- and S-wave arrival times on microseismic data sets. First, time intervals with possible arrivals on waveform recordings are identified using the fuzzy c-means clustering algorithm. Second, these intervals are classified as corresponding to P-, S-, or unidentified waves using the polarization attributes of the waveforms contained within. Third, the P-, S-, and unidentified-waves arrival times are picked using the Akaike information criterion picker on the corresponding intervals. Fourth, unidentified waves are classified as P or S based on the arrivals moveouts. The application of the workflow on synthetic and real microseismic data sets indicates that it yields accurate arrival picks for high and low signal-to-noise ratio waveforms.

Highlights

  • Hypocenter locations are in most cases estimated either using arrival times or waveform-based approaches

  • We illustrate our results in scatter plots of arrival-pick residual against arrival signal-to-noise ratio (SNR)

  • To compute the arrivals SNR, we define a window of noise from the start of the 51 record to one dominant period before the first arrival

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Summary

Introduction

Hypocenter locations are in most cases estimated either using arrival times (e.g., by linearized inversion, grid-search methods; see Buland, 1976; Pavlis, 1986; Moser et al, 1992; Oye and Roth, 2003) or waveform-based approaches (e.g., by time-reverse migration; see Artman et al, 2010; Nakata and Beroza, 2016). Many supervised and unsupervised machine learning methods have gained considerable popularity. Gentili and Michelini (2006) pick P - and S -phases using

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