Comment on “Miocene to Quaternary tectonostratigraphic evolution of the middle section of the Burdur-Fethiye Shear Zone, south-western Turkey: Implications for the wide inter-plate shear zones. Tectonophysics 690, 336-354”

- An attempt to stratigraphy and tectonosedimentary evolution for Çameli Basin has restored.
- A constant deposition from early Miocene onward is proposed without actual age data.
- It conflicts and deviates from the well-articulated stratigraphy and geodynamic.
- We highlight complete marine and terrestrial fossil data for the Çameli Basin area.
- An early-mid Miocene piggy-back basin is superimposed by Vallesian-Villanyian graben.