Carbonate Rocks Origin, Occurrence and Classification by George V. Chilingar, Harold J. Bissell and Rhodes W.

By George V. Chilingar, Harold J. Bissell and Rhodes W. Fairbridge (Eds.)

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252: 683-694. FAIRBRIDGE, R. , 1957. The dolomite question. In: R. J. LEBLANC and J. BREEDMG (Editors), Regional Aspects of Carbonate Deposition ( A Symposium)-Soc. Econ. Paleontol. , Spec. , 5 : 125-178. FAIRBRIDGE, R. , 1964. Theimportance of limestone and its Ca/Mg content to paleoclimatology, In: A. E. M. NAIRN(Editor), Problems in Paleoclimatology. , pp. 431-530. FAIRBRIDGE, R. , 1966. Phases of diagenesis and authigenesis. In: G. LARSEN and G. V. CHILINGAR (Editors), Diagenesis in Sediments.

As pointed out by KUENEN(1950), this event shifted the fundamental site of carbonate sedimentation from shelves to ocean basins (above the “calcium carbonate compensation depth”). From Cretaceous onwards, the carbonates, instead of being limited to shallow epicontinental basins and in part continuously recycled, began to accumulate with more or less continuous burial. It would appear that the Cretaceous Ocean was more extensively saturated or supersaturated with respect to CaC03 than that of today.

1964. Penecontemporary dolomite in the Persian Gulf. Bull. Am. Assoc. Petrol. Geologists, 48: 532-533. IMBRIE,J. and PURDY, E. , 1962. Classification of modern Bahaman carbonate sediments. In: Classification of Carbonate Rocks-Am. Assoc. Petrol. , I : 253-272. , 1962. Problems of the geochemistry of sedimentary carbonate rocks. Geochim. Cosmochim. , 26: 815-847. JANSEN, J. F. ,1963. The resistance of Recent marine carbonate sedinients to solution. J . Oceanog. Soc. Japan, 18: 42-52. , 1959. Manganese in modern and fossil gastropod shells.

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