Seismicity from a dense hydraulic fracturing stimulation monitoring array favors a fluid diffusion mechanism in a low-permeability shale formation in the Montney Basin, British Columbia


Hongyu Yu1, Rebecca M Harrington2, Bei Wang1,3 and YaJing Liu3, (1)Ruhr-Universitat Bochum, Institute of Geology, Mineralogy and Geophysics, Bochum, Germany, (2)Ruhr University Bochum, Institute of Geology, Mineralogy and Geophysics, Bochum, Germany, (3)McGill University, Earth and Planetary Sciences, Montreal, QC, Canada
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