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The Origin of the Girvan-Ballantrae Beerbachites

Published online by Cambridge University Press:  01 May 2009

T. W. Bloxam
T. W. Bloxam
Affiliation:
Dept. of Geological Sciences, University of California, Berkeley, 4, California, U.S.A.
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Abstract

The mode of occurrence and petrography of a group of pyroxene- hornblende-granulites (beerbachites), found only in association with serpentinized peridotite, are described. The beerbachites are regarded as contact altered lavas and basic intrusions which formed the lower levels of a thick series of Ordovician volcanics. Peridotite, intruded into the base of the volcanic pile, disrupted and thermally metamosphosed the lavas and intrusions which appear as inclusions in the serpentinized peridotite. The present contacts between serpentinite and adjacent unmetamorphosed rocks are secondary in origin.

Type
Articles
Information
Geological Magazine , Volume 92 , Issue 4 , August 1955 , pp. 329 - 337
Copyright
Copyright © Cambridge University Press 1955

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References

REFERENCES

Anderson, J. G. C., 1936. Age of the Girvan-Ballantrae Serpentine. Geol. Mag., lxxiii, 535–45.CrossRefGoogle Scholar
Bailey, E. B., and McCallien, W. J., 1952. Ballantrae Problems: Historical Review. Trans. Geol. Soc. Edinb., xv, 14–38.CrossRefGoogle Scholar
Balsillie, D., 1932. The Ballantrae Igneous Complex, South Ayrshire. Geol. Mag., lxix, 107–131.CrossRefGoogle Scholar
Balsillie, D., 1937. Further Observations on the Ballantrae Igneous Complex, South Ayrshire. Geol. Mag., lxxiv, 20–33.CrossRefGoogle Scholar
Beveridge, R., 1950. On the Igneous Rocks of Arenig Age in the Girvan-Ballantrae District, Ayrshire, and their Stratigraphical Relationships. Unpublished Ph. D. Thesis, Library of the University of Edinburgh.Google Scholar
Bloxam, T. W., 1954. Rodingite from the Girvan-Ballantrae Complex, Ayrshire. Miner. Mag. xxx, 525–528.Google Scholar
Campbell, I., and Schenk, E. T., 1950. Camptonite Dykes near Boulder Dam, Arizona. Amer. Min., xxv, 671–92.Google Scholar
MacGregor, A. G., 1931. Scottish Pyroxene-Granulite Hornfelses and Odenwald Beerbachites. Geol. Mag., lxviii, 506–21.CrossRefGoogle Scholar
Ransome, F. L., 1894. The Geology of Angel Island. Bull. Dept. Geol. Univ. Calif., i, 193–235.Google Scholar
Schwartz, G. M., 1924. The Contrast in the Effect of Granite and Gabbro Intrusions on the Ely Greenstone. Journ. Geol., xxxii, 89–138.CrossRefGoogle Scholar
Taliaferro, N. L., 1943. The Franciscan-Knoxville Problem. Bull. Amer. Assn. Pet. Geol., xxvii, 109–219.Google Scholar
Teall, J. J. H., 1899. The Silurian Rocks of Britain, Vol. I, Scotland. Mem. Geol. Surv. Gt. Brit.Google Scholar
Tyrrell, G. W., 1909. A New Occurrence of Picrite in the Ballantrae District and its Associated Rocks. Trans. Geol. Soc. Glasgow, xiii, 283–90.CrossRefGoogle Scholar
Vincent, E. A., 1953. Hornblende-Lamprophyre Dykes of Basaltic Parentage from the Skaergaard Area, East Greenland. Quart. Journ. Geol. Soc., cix, 21–49.CrossRefGoogle Scholar