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New fusulinid evidence for the Permian age of the Palaeozoic rocks of Hydra, Greece
Published online by Cambridge University Press: 01 May 2009
Summary
The Palaeozoic rocks of Hydra consist of a sequence of limestones and dolomites with some interbeds of shales and sandstones. Fusulinid foraminifera indicate the sequence is entirely Permian in age and not Carboniferous and Permian as previously thought.
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