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Figure 5.
Comparison of the pressure-temperature-time (P-T-t) path inferred for the northern Teton Range (thick black dashed line) from Swapp et al. (2018) and P-T-t paths for high-pressure granulites from the eastern syntaxis of the Himalayas compiled by Wang et al. (2017) (red, green, and blue lines). Teton Range P-T conditions determined for the meta-pelitic and mafic gneiss package are indicated by yellow ovals, and P-T conditions determined for the quartzofeldspathic gneiss package are indicated by blue ovals.
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