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Eocene-Oligocene succession at Kıyıköy (Midye) on the Black Sea coast in Thrace
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A belt of Upper Eocene–Lower Oligocene marine sedimentary rocks extends from Kıyıköy on the Black Sea coast to Pınarhisar in the Thrace Basin, suggesting a marine connection between the Black Sea and the Thrace Basin during this period. The Cenozoic succession of this marine corridor was studied in the vicinity of Kıyıköy along two measured stratigraphic sections. The sequence lies unconformably over metamorphic basement rocks and consists of ~75 m of bioclastic limestone and sandstone of the Soğucak Formation, overlain by ~40 m of limestone, marl, mudstone, sandstone, and acidic tuff, which are assigned to the newly defined Servez Formation.
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Journal of Earth Sciences Thrace Basin Black Sea Simplified regional palaeogeographic Palaeogeographic high separating Measured stratigraphic sectionTài liệu liên quan:
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