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A Note on the Progressive Metamorphism of Siliceous Limestones and Dolomites

Published online by Cambridge University Press:  01 May 2009

Extract

The stages of progressive thermal metamorphism of siliceous carbonate sediments covering mineral assemblages revealed in the highest grades of alteration were first delineated by Bowen (1940) in a paper which presented an illuminating systematic treatment of the whole subject. In his account the successive stages in the metamorphism of siliceous limestones and dolomites were, in general, linked with a series of reactions of increasing decarbonation in which thirteen steps were traced, involving the appearance of ten distinct mineral phases. With certain reservations these phases could be accepted as indicators of a temperature grade of metamorphism. Investigations carried out since that time have served to confirm the general validity of the scheme set out which thus brings law and order into a field of metamorphism characterized by considerable mineralogical and petrographical complexity.

Type
Articles
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Agrell, S. O., 1950. A gabbro-limestone contact near Camphouse, Ardnamurchan. Abstracts meeting Miner. Soc. (London), 8th June; also Amer. Min., xxxv, 1080.Google Scholar
Bowen, N. L., 1940. Progressive metamorphism of siliceous limestone and dolomite. Journ. Geol., xlviii, 225274.CrossRefGoogle Scholar
Nockolds, S. R., 1947. On tilleyite and its associated minerals from Carlingford, Ireland. Miner. Mag., xxviii, 151–8.Google Scholar
Tilley, C. E., 1942. Tricalcium disilicate (rankinite), a new mineral from Scawt Hill, Co. Antrim. Miner. Mag., xxvi, 190–6.Google Scholar
Tilley, C. E., 1947. The gabbro-limestone contact zone of Camas Mòr, Muck, Inverness-shire. Compt. Rend. Soc. Geol. Finlande, xx, 97105.Google Scholar
Tilley, C. E., 1948. Earlier stages in the metamorphism of siliceous dolomites. Miner. Mag., xxviii, 272–6.Google Scholar
Zambonini, F., 1935. Mineralogia Vesuviana, 2nd edit., by Quercigh, E., Naples, p. 66.Google Scholar