|
2. Neoththys: Levant and North African offshore |
Geological Survey of Israel, Malkhei Yisrael Street 30, 95501 Jerusalem, Israel
The Mesozoic facies, distribution, palaeo-zoo-geography and tectonic history of the Levantine and Tauride-Zagride autochthonous and para-autochthonous units, suggest that these areas were part of the Arabian sub-plate and never lay far apart. This would tend to invalidate the hypothesis of an oceanic basin (Mesogea) in the present Eastern Mediterranean during the Mesozoic.
This article has been cited by other articles:
![]() |
A. H. F. Robertson, J. E. Dixon, S. Brown, A. Collins, A. Morris, E. Pickett, I. Sharp, and T. Ustaomer Alternative tectonic models for the Late Palaeozoic-Early Tertiary development of Tethys in the Eastern Mediterranean region Geological Society, London, Special Publications, 1996; 105: 239 - 263. [Abstract] [PDF] |
||||