Page 23 - Carbonate Platforms Facies, Sequences, and Evolution

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Fig. 6. Arid platform. Lower Cambrian Laminated Dolomite (above) and Upper Triassic Boccheggiano Anhydrite (below).
tectonic deformation resulting from the former occurrence of sulphates. (b) Pseudomorphs of sulphate nodules in ea
laminite and anhydrite layers tectonically deformed by the plastic behaviour of sulphates. (d) Anhydrite nodules a