2015
DOI: 10.1016/j.jsg.2015.11.001
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Orientation, composition, and entrapment conditions of fluid inclusions in the footwall of the northern Snake Range detachment, Nevada

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Cited by 6 publications
(3 citation statements)
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References 104 publications
(149 reference statements)
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“…9). This interpretation is consistent with the results of experimental deformation of fluid inclusions enclosed in quartz grains (Tarantola et al, 2010(Tarantola et al, , 2012, with recent work from the Snake range quartzite detachment (Carter et al, 2015) where similar features have been documented and with the localization of fluid inclusion trails along deformation bands (Wilkins and Barkas, 1978). According to this interpretation, the curved geometry of most inclusion trails suggests that they have been deformed after their formation.…”
Section: Intracrystalline Deformation and Fluid Redistributionsupporting
confidence: 91%
“…9). This interpretation is consistent with the results of experimental deformation of fluid inclusions enclosed in quartz grains (Tarantola et al, 2010(Tarantola et al, , 2012, with recent work from the Snake range quartzite detachment (Carter et al, 2015) where similar features have been documented and with the localization of fluid inclusion trails along deformation bands (Wilkins and Barkas, 1978). According to this interpretation, the curved geometry of most inclusion trails suggests that they have been deformed after their formation.…”
Section: Intracrystalline Deformation and Fluid Redistributionsupporting
confidence: 91%
“…Brittle failure leads to the formation of faults, fractures and microcracks, which allow for surface fluids to be pumped into the shear zone (Fig. 11b; Sibson, 1977;McCaig, 1988;Lister & Davis, 1989;Carter et al 2015;Siebenaller et al 2016;Compton et al 2017;Prando et al 2020;Menegon & Fagereng, 2021). After rupture, during post-seismic relaxation, stress decays and the detachment shear zone re-enters the dislocation creep regime.…”
Section: C Model For Fluid Circulationmentioning
confidence: 99%
“…Deformation at the brittle-ductile transition is cyclical, oscillating between brittle and ductile behaviour (e.g. Famin et al 2004Famin et al , 2005Siebenaller et al 2013Siebenaller et al , 2016Carter et al 2015;Compton et al 2017). A switch in failure mode is typically attributed to a perturbation in one of the parameters controlling deformation, such as deviatoric stress, strain rate or pore fluid pressure.…”
Section: Introductionmentioning
confidence: 99%