GSA Annual Meeting in Phoenix, Arizona, USA - 2019

Paper No. 199-14
Presentation Time: 9:00 AM-6:30 PM

THE CLUMPED-ISOTOPE GEOCHEMISTRY OF EXHUMED SHEAR ZONE IN CARBONATE ENVIRONMENT: EXAMPLES FROM THE TORNGAT OROGEN (CANADA)


LACROIX, Brice J.1, TRAP, Pierre2, VENNEMANN, Torsten3, DURAND, Cyril4, GONCALVES, Philippe2 and MARQUER, Didier2, (1)Geology, Kansas State University, 110 Anderson Hall, 919 Mid Campus Drive North, Manhattan, KS 66506, (2)UMR Chrono-environnement, Université de Franche-Comté, 16 route de Gray, Besançon, 25030, France, (3)Institute of Earth Surface Dynamics, University of Lausanne, Geopolis - CH-1015 Lausanne - Suisse, Lausanne, 1015, Switzerland, (4)Departement des Sciences de la Terre, Université de Lille 1, Villeneuve d’Ascq, 59655, France

Clumped isotope thermometry is a technique that ideally recovers the temperature of carbonate formation without the need to assume the composition of precipitating water and/or oxygen composition of another mineral phase, as is required for conventional stable isotope thermometry. However, applications of this technique to high-grade metamorphic conditions are sparse. Here, we present new single- (O and C) and clumped- (∆47) isotopes compositions measured across sheared marbles from the Torngat orogen, Canada, to explore how retrograde metamorphic reactions /deformation may affect ∆47 compositions. Clumped isotope compositions of the host dolomite marbles record apparent peak metamorphic equilibrium temperatures of 300-500˚C. Although these temperatures are significantly lower compared to peak temperature derived from C-isotope equilibrium between carbonate and graphite (~725˚C), and from metamorphic reactions (~750˚C), they are higher than other apparent ∆47 temperatures of dolomitic marbles elsewhere (e.g. metamorphic core-complex of Naxos, Notch Peak aureole). Surprisingly, ∆47 temperatures recorded along the shear zone are virtually very low, giving temperatures as low as 0˚C. Our petrographic investigations show that shear zones are associated with local dissolution of carbonate grains and the apparition of amphiboles. Both metamorphic assemblage and C-isotope equilibrium between carbonate and graphite suggest that shear zones formed during retrograde conditions at temperatures in the range 550-625˚C. Our results suggest that ∆47 doesn’t record the absolute peak temperature experienced by marbles. However, the abrupt change in ∆47 values across the shear zone may suggest 1) a possible kinetic exchange of C and O between carbonate and newly-formed amphiboles, 2) strain or dynamic recrystallization, or 3) fluid-rock interaction.