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Publications by [Karkitsios V.]
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<p>The main orogenic movements took place at the end of the Burdigalian (IGRS-IFP, 1966). The Ionian basin evolution constitutes a good example of inversion tectonics of a basin with evaporitic base (Karakitsios, 1995): the double divergence of the basin (westwards ...
Filed under:
Geology -
Economic Geology
Reference:
AAPG International Conference Barcelona, Spain 2003
