1887

Abstract

Recorded microseismic waveforms during hydraulic fracture monitoring are usually complex wavetrains contaminated by high amplitude noise. This makes difficult to accurately estimate the onset time of the various recorded arrivals. In this paper we propose

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/content/papers/10.3997/2214-4609.201400407
2009-06-08
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400407
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