作者: Catherine Kissel , Carlo Laj , Alain Mazaud
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摘要: Paleomagnetic results from Neogene volcanic and sedimentary formations in central Aegea indicate that Evia Skyros have undergone a 48° 26° clockwise rotation respectively. The Volos region does not show any significant the last 3 Ma. of is about twice as large one measured coeval external Hellenic arc. are interpreted terms published model distributed deformation by faulting, which also provides an explanation for differential Skyros.