2008
DOI: 10.1016/j.gca.2008.08.012
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Age trends in garnet-hosted monazite inclusions from upper amphibolite facies schist in the northern Grouse Creek Mountains, Utah

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Cited by 39 publications
(36 citation statements)
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References 77 publications
(158 reference statements)
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“…6 and 7;Holdaway, 1971; for an alternative interpretation of the ages of these metamorphic mineral assemblages, see Wells et al, 2012). Asymmetric fabrics and lineations, defi ned (in part) by the growth of elongate bundles of fi brolitic sillimanite, indicate top-to-the-northwest shear during northwest-southeast stretching at amphibolite facies conditions, leading us to conclude that the rise and emplacement of the Oligocene Cassia plutonic complex was intimately related to the dominant deformational and metamorphic event mapped in its country rocks (Strickland et al, 2011a(Strickland et al, , 2011b (Saltzer and Hodges, 1988;Wells et al, 2000) that were interpreted as recording on April 3, 2013 geosphere.gsapubs.org Downloaded from initial cooling of footwall rocks during Eocene motion along the Middle Mountain shear zone (Saltzer and Hodges, 1988;Wells et al, 2000;Hoisch et al, 2008).…”
Section: Geology and Geochronology Of Footwall Rocks Of The Argmentioning
confidence: 89%
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“…6 and 7;Holdaway, 1971; for an alternative interpretation of the ages of these metamorphic mineral assemblages, see Wells et al, 2012). Asymmetric fabrics and lineations, defi ned (in part) by the growth of elongate bundles of fi brolitic sillimanite, indicate top-to-the-northwest shear during northwest-southeast stretching at amphibolite facies conditions, leading us to conclude that the rise and emplacement of the Oligocene Cassia plutonic complex was intimately related to the dominant deformational and metamorphic event mapped in its country rocks (Strickland et al, 2011a(Strickland et al, , 2011b (Saltzer and Hodges, 1988;Wells et al, 2000) that were interpreted as recording on April 3, 2013 geosphere.gsapubs.org Downloaded from initial cooling of footwall rocks during Eocene motion along the Middle Mountain shear zone (Saltzer and Hodges, 1988;Wells et al, 2000;Hoisch et al, 2008).…”
Section: Geology and Geochronology Of Footwall Rocks Of The Argmentioning
confidence: 89%
“…These earlier conclusions are supported by geo chronologic studies (Egger et al, 2003;Strickland et al, 2011aStrickland et al, , 2011b. Alternatively, studies by Wells et al (1998Wells et al ( , 2012, Harris et al (2007), Hoisch et al (2008), and used metamorphic pressure-temperature estimates in conjunction with geochronol-ogy and thermochronology to argue that many of the high-strain fabrics in the Grouse Creek and Albion Mountains are related to alternating periods of contraction and extension in Cretaceous-Eocene time.…”
Section: Introductionmentioning
confidence: 94%
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“…Emerging developments in linking 'age to stage', and particularly the use of combined petrography and traceelement data from major and accessory phases (petrochronology), allow high-spatial precision geochronological data to be more firmly linked to the P -T conditions of accessory phase crystallisation reactions (Foster et al, 2004;Gasser et al, 2012;Janots et al, 2008;Rubatto et al, 2013). This is achieved by detailed observation of textural relationships, geochemical analysis of coexisting accessory phases and systematic documentation of trace-element signatures in major phases that 'fingerprint' monazite-forming reactions (Foster et al, 2002(Foster et al, , 2000(Foster et al, , 2004Gasser et al, 2012;Hermann and Rubatto, 2003;Hoisch et al, 2008;Janots et al, 2006Janots et al, , 2007Janots et al, , 2008Janots et al, , 2009Kingsbury et al, 1993;Pyle and Spear, 2003;Rubatto et al, 2006;Smith and Barreiro, 1990;Spear, 2010;Wing et al, 2003). Such advances in metamorphic and geochronological analysis offer the potential to unravel the complex tectonic and thermal evolution of thrust zones associated with inverted metamorphism.…”
Section: Introductionmentioning
confidence: 99%
“…The presence of inclusions of one phase within a host mineral representing a different phase has been exploited to gain insight into the pressure-temperature-compositiontime-deformation (P-T-X-t-D) evolution in studies of igneous and metamorphic systems (e.g., Chopin 1984;Van der Molen and Van Roermund 1986;St-Onge 1987;Perrillat et al 2003;Hoisch et al 2008;Ashley et al 2014). For example, St-Onge (1987) analyzed biotite and plagioclase inclusions from core to rim in garnet to estimate pressure and temperature evolution with net transfer barometry and exchange thermometry, respectively.…”
Section: Introductionmentioning
confidence: 99%