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The Glen Dessarry Marble and its Associated Calc-Silicate Rocks.

Published online by Cambridge University Press:  01 May 2009

W. T. Harry
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Abstract

White marble in Glen Dessarry, West Highlands of Scotland, occurs as three lenses associated with schists and calc-silicate rocks. The minerals identified in all these rocks are apatite, biotite, calcite, chondrodite, clinochlore, clinozoisite, diopsidic-pyroxene, dolomite, epidote, forsterite, garnet, hornblende, magnetite, phlogopite, plagioclase, potash-feldspar, pyrites, quartz, scapolite, sillimanite, sphene, vesuvianite, zoisite.

Two parageneses may be distinguished. One, due to high-grade regional metamorphism, apparently with little or no introduction of material, is a diopsidic-pyroxene, forsterite, phlogopite, calcite, dolomite association forming white marble. The other association occurs as veinlets and small irregular bodies in the white marble. It appears to be due to circulating solutions in which pyroxene and forsterite were unstable. Minerals of this paragenesis include potash-feldspar, plagioclase, scapolite, hornblende, minerals of the epidote group, calcite, and quartz. In certain localities scapolite formed at the expense of plagioclase and was succeeded by crystallization of epidote.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 6 , December 1951 , pp. 393 - 403
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Bowen, N. L., 1940. Progressive metamorphism of siliceous Limestone and Dolomite. Journ. Geol., xlviii, 225–274.CrossRefGoogle Scholar
Bruce, E. L., and Russell, G. A., 1939. Petrography of the crystalline limestones and quartzites of the Grenville series. Bull. Geol. Soc. Amer., 1, 515–528.CrossRefGoogle Scholar
Clarke, F. W., 1924. The Data of Geochemistry. U.S. Geol. Sur. Bull., 770.Google Scholar
Davidson, C. F., 1943. The Archaean Rocks of the Rodil District, South Harris, Outer Hebrides. Trans. Roy. Soc. Edinburgh, lxi, 71–112.Google Scholar
Eckermann, H. von, 1922. Rocks and Minerals of the Mansjö Mountain. Geol. För. Förh., xliv, 203–410.CrossRefGoogle Scholar
Hallimond, A. F., 1926. On the chemical classification of the mica group. II—The basic micas. Miner. Mag., xxi, 25–33.Google Scholar
Read, H. H., and Double, I. S., 1935. On the occurrence of chondrodite in the Glenelg limestone of Inverness-shire. Miner. Mag., xxiv, 84–9.Google Scholar
Rosenholtz, J. L., and Smith, D. T., 1950. Crestmore sky blue marble, its linear thermal expansion and color. Amer. Miner., xxxv, 1049–1054.Google Scholar
Shazli, E. M., 1950. The application of the spectrographic analysis of minerals to the metallogenesis of lead-zinc ores. Unpublished thesis Geol. Dept. Imp. Coll. Sci. and Tech.Google Scholar
Tilley, C. E., 1923. The Metamorphic Limestones of Commonwealth Bay, Adelie Land. Australasian Antarctic Exped. Sci. Rep., Ser. A, iii.Google Scholar
Turner, F. J., 1948. Mineralogical and structural evolution of the metamorphic rocks. Geol. Soc. Amer. Mem., xxx.Google Scholar