Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (<250 to >1000 °C/GPa) explained by tectonic plate convergence in deep time

Allen P. Nutman*, Vickie C. Bennett, Clark R.L. Friend, Keewook Yi

*Corresponding author for this work

    Research output: Contribution to journal › Article › peer-review

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    Earth and Planetary Sciences