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The study investigates the coal characteristics and biomarker composition of the Dombayova coals from the Late Miocene to Pliocene age in western Turkey. It reveals that the coal is primarily composed of weakly altered wood fragments and roots, with significant contributions from terrestrial plants, indicating a high density of Betulaceae in the peat-forming vegetation. The findings also suggest environmental changes during peat formation, influenced by fluctuating water levels and alkaline conditions in th

Author

Syahronidavi Al Ghifari

Language

EN