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kaberettI do not particularly care to confess to any or all of (i) how long this took me, (ii) how much longer I'm considering spending on it, and (iii) what I should arguably have been doing instead for the last several days. Nevertheless: BEHOLD.
[A graph showing Tl concentration and isotope ratios for lavas from the Aleutian arc (Nielsen et al. 2016), Mariana arc (Prytulak et al. 2013, 2017), Ryukyu-Okinawa arc [circles] and back-arc basin [diamonds] system (Shu et al. 2017), Tonga-Kermadec arc (Nielsen et al. 2017), and Central American Volcanic Arc (Nielsen et al. 2017). For oceanic arcs (left) "C." = "Central"; "M." = "Middle"; "v.f." = "volcanic front". For the CAVA (right), "C." = "Cerro". The dotted line on Tl isotope ratio panels indicates estimated average mantle ε205Tl (= -2 ± 1). Error bars are smaller than symbolsexcept for low-concentration samples, where I need to look up uncertainties and edit them in, sob.]
[A graph showing Tl concentration and isotope ratios for lavas from the Aleutian arc (Nielsen et al. 2016), Mariana arc (Prytulak et al. 2013, 2017), Ryukyu-Okinawa arc [circles] and back-arc basin [diamonds] system (Shu et al. 2017), Tonga-Kermadec arc (Nielsen et al. 2017), and Central American Volcanic Arc (Nielsen et al. 2017). For oceanic arcs (left) "C." = "Central"; "M." = "Middle"; "v.f." = "volcanic front". For the CAVA (right), "C." = "Cerro". The dotted line on Tl isotope ratio panels indicates estimated average mantle ε205Tl (= -2 ± 1). Error bars are smaller than symbols