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

Citation

Nutman, A, Bennett, V, Friend, C et al. 2020, 'Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (< 250 to > 1000 degrees C/GPa) explained by tectonic plate convergence in deep time', Precambrian Research, vol. 344, pp. 1-17.

Year

2020

ANU Authors

Fields of Research

  • Geochronology
  • Tectonics

Updated:  20 April 2024 / Responsible Officer:  Director (Research Services Division) / Page Contact:  Researchers