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Abstract

Shear waves from microearthquakes induced by hydraulic fracturing are observed on three-component (3C) accelerometers along a 2 km surface profile. The S-wave waveforms exhibit at least two distinct phases suggesting shear-wave splitting. This observation

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/content/papers/10.3997/2214-4609.201400499
2009-06-08
2021-10-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400499
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