Jump to content

Goianides Ocean

From Wikipedia, the free encyclopedia

The Goianides Ocean was an ocean that existed in South America in Neoproterozoic times. It separated the Paranapanema block and the São Francisco Craton. Its closure started with a magmatic arc forming (now seen as granitoids of the Guaxupé and Socorro Nappes) and eventually gave rise to the Brasiliano orogeny.[1]

See also

[edit]

References

[edit]
  1. ^ "Journal of the Virtual Explorer | A dynamic review electronic Earth Science journal publishing material from all continents". Archived from the original on 2019-04-06. Retrieved 2018-07-07.