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dc.contributor.authorCebry, Sara B. L.
dc.contributor.authorKe, Chun-Yu
dc.contributor.authorMcLaskey, Gregory C.
dc.date.accessioned2022-05-19T15:29:23Z
dc.date.available2022-05-19T15:29:23Z
dc.date.issued2022-05
dc.identifier.urihttps://hdl.handle.net/1813/111278
dc.description.abstractThese files contain data supporting all results reported in: "The Role of Background Stress State in Fluid-Induced Aseismic Slip and Dynamic Rupture on a 3-meter Laboratory Fault" by Cebry et al., where we found: Fluid injection stimulates seismicity far from active tectonic regions, however the details of how fluids modify on-fault stresses and initiate seismic events remains poorly understood. We conducted laboratory experiments using a biaxial loading apparatus with a 3 m saw-cut granite fault and compared events induced at different background shear stress levels. Water was injected at 10 ml/min and normal stress was constant at 4 MPa. In all experiments, aseismic slip initiated on the fault near the location of fluid injection and dynamic rupture eventually initiated from within the aseismic slipping patch. When the fault was near critically stressed, seismic slip initiated only seconds after MP a-level injection pressures were reached and the dynamic rupture propagated beyond the fluid pressure perturbed region. At lower stress levels, dynamic rupture initiated hundreds of seconds later and was limited to regions where aseismic slip had significantly redistributed stress from within the pressurized region to neighboring locked patches. We find that slow slip initiated when local stresses exceeded Coulomb failure criteria, but initiation of dynamic rupture required additional criteria to be met. Even high background stress levels required aseismic slip to modify on-fault stress to meet initiation criteria. We also observed slow slip events prior to dynamic rupture. Overall, our experiments suggest that initial fault stress, relative to fault strength, is a critical factor in determining whether a fluid-induced rupture will "runaway" or whether a fluid ­induced rupture will remain localized to the fluid pressurized region.en_US
dc.description.sponsorshipNational Science Foundation Grant EAR- 184 7139en_US
dc.language.isoen_USen_US
dc.relation.isreferencedbyCebry, S. B. L., Ke, C.-Y., and McLaskey, G. C. (2022) Data from: The role of background stress state in fluid-induced aseismic slip and dynamic rupture on a 3-meter laboratory fault, JGR: Solid Earth, submitted.
dc.rightsCC0 1.0 Universal*
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/*
dc.subjectInduced seismicityen_US
dc.subjectfluid injectionen_US
dc.subjectaseismic slipen_US
dc.subjectlaboratory experimentsen_US
dc.subjectbackground stressen_US
dc.subjectinitiationen_US
dc.titleData from: The Role of Background Stress State in Fluid-Induced Aseismic Slip and Dynamic Rupture on a 3-meter Laboratory Faulten_US
dc.typedataseten_US
dc.identifier.doihttps://doi.org/10.7298/gdxn-e175


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