Page 28 - Carbonate Platforms Facies, Sequences, and Evolution

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Fig. 7. Humid platform. Lower Cambrian Ceroide Limestone (right) and Lower Liassic Massiccio Limestone (left)
algae (Epiphyton) and archaeocyathids. (c), (d) Oolitic grainstone; larger coated grains and skeletal remain
deformed. (e), (f) Fenestral fabric in stromatolitic boundstone, irregular fenestrae are filled by two gener
and grapestone lumps; peloids and skeletal remains are associated with the Jurassic facies.
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