Plots of TiO2-Zr (upper) and Y-Zr (lower) for mafic volcanic rocks in at Hidden Creek, Anyox, indicating that they are mainly MORB-type basalts and basaltic andesities of tholeiite affinity, although some enriched (E-MORB-type) basalts are also present (Macdonald et al. 1996).





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