JOURNAL OF METAMORPHIC GEOLOGY, vol.12, no.4, pp.455-466, 1994 (SCI-Expanded)
The north-west Turkish blueschists of represent a subducted passive continental margin sequence dominated by metaclastic rocks and marble. T. depositional age of the blueschist protoliths are probably Palaeozoic to Mesozoic, while the age of the high-pressure/low-temperature metamorphism is Late Cretaceous. Blueschists are tectonically overlain by a volcanosedimentary sequence made up of accreted oceanic crustal material that locally shows incipient blueschist metamorphism and by spinel peridotite slices.