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  4. An improved method for hydrofracture induced microseismic event detection and phase picking

An improved method for hydrofracture induced microseismic event detection and phase picking

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Author(s)
Song, Fuxian
•
Kuleli, Huseyin Sadi
•
Toksoz, M. Nafi
•
Ay, Erkan
•
Zhang, Haijiang
Date Issued
2010
Publisher
Massachusetts Institute of Technology. Earth Resources Laboratory
Series/Report no.
Earth Resources Laboratory Industry Consortia Annual Report;2010-12
Abstract
The ability to detect small microearthquakes and identify their P and S phase arrivals is a key issue in hydrofracture downhole monitoring because of the low signal-to-noise ratios. We apply an array-based waveform correlation approach (matched filter) to improve the detectability of small magnitude events with mechanisms and locations similar to a nearby master event. After detecting the weak events, we use a transformed spectrogram method to identify the phase arrivals. We have tested the technique on a downhole monitoring dataset of the microseismic events induced by hydraulic fracturing. We show that, for this case, one event with a signal-to-noise ratio around 6dB, which is barely detectable using an array-stacked short-time average/long-time average (STA/LTA) detector under a reasonable false alarm rate, is readily detected on the array-stacked correlation traces. The transformed spectrogram analysis of the detected events improves P and S phase picking.
Subjects
Microseismic
Persistent DSpace Link
http://hdl.handle.net/1721.1/68587
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