Ordovician-Silurian rift-passive margin on the Mexican margin of the Rheic Ocean overlain by Carboniferous-Permian periarc rocks: Evidence from the eastern Acatlan Complex, Southern Mexico

Citation

Morales-Gámez, M, Keppie, J & Norman, M 2008, 'Ordovician-Silurian rift-passive margin on the Mexican margin of the Rheic Ocean overlain by Carboniferous-Permian periarc rocks: Evidence from the eastern Acatlan Complex, Southern Mexico', Tectonophysics, vol. 461, no. 1-4, pp. 291-310.

Year

2008

ANU Authors

Fields of Research

  • Tectonics
  • Geochronology

Updated:  27 July 2024 / Responsible Officer:  Director (Research Services Division) / Page Contact:  Researchers