An apatite for progress: Inclusions in zircon and titanite constrain petrogenesis and provenance

Abstract : Apatite has recently gained considerable attention as a mineral with many uses within the Earth and planetary sciences. Apatite chemistry has recently given new insight into a wide range of geological processes and tools, for example, magmatism, metasomatism, planetary geochemistry, and geochronology. We expand the utility of apatite here by presenting a novel way to fingerprint magma chemistry and petrogenesis using apatite inclusions within robust titanite and zircon. We present trace element data from apatite mineral inclusions shielded within magmatic zircon and titanite. Importantly, apa-tite inclusion and host titanite chemistries detailed in this study allow estimation of the whole-rock Sr and SiO 2. We show how these data can be used to assess the degree of fractionation of the host magma and to calculate key trace element abundances and ratios. We demonstrate that the inclusions can be linked to discrete periods in the crystalliza-tion history of the host phases, thus providing insight into petrogene-sis. The results highlight that apatite compositions might discriminate modern granitoids (younger than 2.5 Ga) from Archean-Proterozoic transitional granitoid compositions (sanukitoid signatures). Development of such a petrological tool has important potential for interpretation of provenance and a better understanding of the secular evolution of the continental crust, including that of early Earth.
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Emilie Bruand, Craig Storey, Mike Fowler. An apatite for progress: Inclusions in zircon and titanite constrain petrogenesis and provenance. Geology, Geological Society of America, 2016, 44 (2), pp.91-94. ⟨10.1130/G37301.1⟩. ⟨hal-02347154⟩



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