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Zonguldak basin : ウィキペディア英語版 | Zonguldak basin The Zonguldak basin of North Western Turkey has been mined for coal since the late 1800s. The basin takes its name after Zonguldak, Turkey, and is approximately 41° N. The Zonguldak basin is the only basin in Turkey with minable coal deposits. Geographically, the Zonguldak is roughly elliptical in shape with its long axis oriented roughly SW – NE, and is adjacent to the Black Sea. Three main regions have been recognized in the Zonguldak basin. These are the Armutcuk, the Zonguldak, and the Amasra from west to east respectively.〔Sinayuç, C., and Gümrah, F. (2009) Modeling of ECBM recovery from Amasra coalbed in Zonguldak Basin, Turkey, International Journal of Coal Geology, 77, 162-174〕 ==Depostional history==
The Zongdulak basin has undergone two major periods of deposition. The first period of deposition began in the Paleozoic and the second began in the Cretaceous. Isolated areas of deposition in the basin occurred during the Late Permian through the Triassic and the Latest Jurassic.
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