Linking titanite U–Pb dates to coupled deformation and dissolution–reprecipitation
نویسندگان
چکیده
Abstract Titanite U–Pb geochronology is a promising tool to date high-temperature tectonic processes, but the extent and mechanisms by which recrystallization resets titanite dates are poorly understood. This study combines dates, trace elements, zoning, microstructures directly deformation fluid-driven along Coast shear zone (BC, Canada). Twenty grains from deformed calc-silicate gneiss yield that range ~ 75 50 Ma. Dates between 60 Ma represent metamorphic crystallization or inherited detrital cores, whereas reflect localized, grain-scale processes variably recrystallized titanite. All analyzed show evidence of fluid-mediated dissolution–reprecipitation, particularly at grain rims, lack thermally mediated volume diffusion temperature > 700 °C. The younger predominantly found in bent portions fluid-recrystallized rims. These features likely formed during ductile slip associated fluid flow zone, although it unclear whether 10 Myr continuous incomplete resetting system punctuated event. Correlations trace-element concentrations vary, indicating effects dissolution–reprecipitation decoupled some grains. results demonstrate lattices subgrains may crystal-plastic deformation, suggesting enhance recrystallization, emphasize complexity within among individual
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ژورنال
عنوان ژورنال: Contributions to Mineralogy and Petrology
سال: 2022
ISSN: ['1432-0967', '0010-7999']
DOI: https://doi.org/10.1007/s00410-022-01906-9