Thrace Basin basement, comprises interbedded fine to coarse grained clastics from a variety of depositional environments, turbidite, muddy carbonates with local reef developments, river channels and tuffs. More than 400 wells were drilled till 2008; 14 gas and 3 oil fields were discovered and all of them are producing. Main gas productions zones are between Eocene- Oligocene deposits; Hamitabat (turbiditic sandstones), Ceylan (tuffs), Sogucak (reefal limestone), and Osmancik (deltaic sandstone) formations. Shales of Hamitabat and Mezardere formations have good source potentials. Thrace Basin The European side of Turkey is called the Thrace Basin. It is the largest and thickest Cenozoic sedimentary basin
1934 Thrace pogroms foreign diplomats of the time saw the government as implicitly supporting the Thrace pogrom in order to facilitate the relocation of the Jewish population. 1934 Thrace pogroms The 1934 Thrace pogroms () refers to a series of violent attacks against Jewish citizens of Turkey in June and July 1934 in the Thrace region of Turkey. According to Corry Guttstadt, a "crucial factor" behind the events was the 1934 Turkish Resettlement Law passed by the Turkish Assembly on 14 June 1934. The pogroms occurred in Tekirdağ, Edirne, Kırklareli, and Çanakkale, and were motivated by anti-Semitism. Some have argued the acts were