Fig. 12
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Histograms and density distribution of temperatures for magmatic Furongian–Lower Ordovician grains and rims of the Cézarenque–Joyeuse gneisses, obtained via the Ti-in zircon thermometer using the equation of Ferry and Watson (2007) with aSiO2 of 1 and aTiO2 of 0.5 as suggested by Schiller and Finger (2019) for peraluminous felsic magmas.
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