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. 2016 Oct 31;113(49):13959–13964. doi: 10.1073/pnas.1616129113

Fig. 3.

Fig. 3.

(A) Zircon U-Th model ages (ka) vs. Ti-in zircon temperatures for cogenetic enclaves Gran 1.1 (spike recorded) and SLJL52 (no spike recorded). (B) Correlation between the extent of spike recorded and Zr whole rock abundance (δT °C is maximum − minimum temperature recorded in each enclave).