Bedrock testing of zircon annealing for detrital provenance studies: Raman and U-Pb analysis in the Adamello batholith (Southern Alps, Italy)

We present a new conceptual model for the interpretation of bedrock and detrital zircon data based on a comparison between theoretical alpha-damage inferred from U-Pb data and actual alpha-damage measured by Raman analysis. The model is tested in the Cenozoic Adamello composite batholith in the Southern Alps (Italy), a natural laboratory where the progressive emplacement of successive magmatic bodies has thermally affected both the metamorphic country rocks and the previously emplaced igneous rocks under well-constrained geological conditions. Bedrock samples were collected along a traverse that spans the contact between plutons of different ages and their country rocks. We found that: (i) zircon rims from the Adamello batholith invariably show a complex, but consistent annealing history after crystallization, as induced by subsequent intrusion of younger plutonic bodies; (ii) zircon cores record damage accumulation starting from the age of rim crystallization; (iii) the severity of annealing in country rock zircons correlates with distance from the nearby plutons. Results on bedrock zircon are then exported to a synthetic detrital zircon population to test how the impact of reheating can be detected in detritus. We found that the application of our model allows increasing the resolution of provenance discrimination, providing a level of information approaching the evolution inferred from bedrock data. We conclude that an approach to detrital zircon geochronology complementing detrital U-Pb ages with Raman spectroscopy could open new venues in sediment provenance analysis and could be proficiently used to improve the identification of clastic detritus sources.