Nontrivial clustering of microseismicity induced by hydraulic fracturing
For induced microseismicity associated with hydraulic fracturing, the frequency‐magnitude distribution is typically characterized by a falloff with increasing magnitude that is significantly faster than for seismicity along active fault systems. This characteristic may arise from a break in scale in...
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Veröffentlicht in: | Geophysical research letters 2016-10, Vol.43 (20), p.10,672-10,679 |
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