Oceanisation

Process of formation of an ocean after continental rifting.The oceanisation is marked by the accretion of oceanic basalts between the drifting continental blocks and the incursion of marine waters and species in the rift basin.[1][2]

References

  1. ↑ Abbate, Ernesto. Oceanisation processes and sedimentary evolution of the Northern Apennine ophiolite suite: a discussion. 1994.
  2. ↑ Brunn, J. H. "Ophiolites, origins of orogens and oceanisation." Ophiolites Proceedings of the International Symposium, Cyprus. 1979.
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