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007	cr |n|||||||||
008	260210t20162016oncda   ob   f|0| 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn---
086	1 |aM183-2/8028E-PDF
100	1 |aLaRochelle, S., |eauthor.
245	10|aPoroelastic modeling of hydraulic fracturing induced earthquake stress field / |cS. Larochelle, Y. Liu, and H. Kao.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2016.
264	4|c©2016
300	|a1 online resource (27 pages) : |bcharts, illustrations.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v8028
504	|aIncludes bibliographical references (pages 16-17).
520	|a"In this study, poroelasticity is implemented in a numerical model of the problem at stake by using the finite-difference software FLAC3D (ITASCA, 2011) supported by the Geological Survey of Canada (GSC) Induced Seismicity Research Project. Given a fixed injection source near a pre-existing fault, this preliminary model simulates slip as well as stresses and pore pressure evolution in the vicinity of the fault. The model is informed by hydraulic fracturing induced seismic events of the Crooked Lake Sequences in Western Canada (Schultz et al., 2015). The present report is part of a larger research initiative which aims to quantify aseismic and seismic fault slip induced by fluid injections associated with hydraulic fracturing operations (Liu et al., 2015)"--page 4.
650	0|aHydraulic fracturing.
650	0|aInduced seismicity.
650	6|aFracturation hydraulique.
650	6|aTremblements de terre provoqués.
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|v8028.|w(CaOODSP)9.506878
856	40|qPDF|s4.15 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-8028-eng.pdf
856	4 |qHTML|sN/A|uhttps://doi.org/10.4095/297811