Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-29T11:48:35.353Z Has data issue: false hasContentIssue false
  • English
  • Français

Serpentinites in the North-East Ox Mountains, Eire

Published online by Cambridge University Press:  01 May 2009

G. G. Lemon
G. G. Lemon
Affiliation:
Department of Geology, University College, Cathays Park, Cardiff.
Get access Rights & Permissions [Opens in a new window]

Abstract

Six serpentinites occur in the Moinian granulites of the North-East Ox Mountains. Four have been known for some time and have been previously described. Additional information on these and the associated vermiculite deposits is provided. The remaining two serpentinites are described for the first time. A pyroxenite vein associated with one of these may have been produced by meta-morphic regeneration.

The relationship of some of these serpentinites to the probable position of the Highland Boundary Fracture-zone in Eire is also discussed. Brief comparison is made with serpentinites occurring in the Scottish Moinian.

Type
Articles
Information
Geological Magazine , Volume 103 , Issue 2 , April 1966 , pp. 124 - 137
Copyright
Copyright © Cambridge University Press 1966

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Anderson, J. G. C., 1947. The Geology of the Highland Border: Stonehaven to Arran. Trans. roy. Soc. Edin., 61, 479–515.CrossRefGoogle Scholar
Anderson, J. G. C., 1960. The Wenlock Strata of South Mayo. Geol. Mag., 97, 265–275.CrossRefGoogle Scholar
Bishopp, D. W., 1946. The Occurrence of Nickel and Magnetite in some Irish Serpentines, in conjunction with a Magnetic Survey. Sci. Proc. Roy. Dublin. Soc. N.S., 24, 125–133.Google Scholar
Bowen, N. L., and Tuttle, O. F., 1949. The System MgO-SiO2-H2O. Bull. geol Soc. Amer., 60, 439–460.CrossRefGoogle Scholar
Cole, G. A. J., 1903. The Intrusive Gneiss of Tirerrill and Dromahaire. Proc. roy. Irish. Acad., 24, B, p. 361.Google Scholar
Cole, G. A. J., 1913. The Geology of the Mallaranny and Sligo District. Proc. Geol. Ass., 24, 62–69.CrossRefGoogle Scholar
Currall, A. E., 1963. The Geology of the S.W. end of the Ox Mountains, Co. Mayo. Proc. roy. Irish Acad., 63, B, 131–165.Google Scholar
Deer, W. A., Howie, R. A., and Zussman, J., 1962. Rock Forming Minerals. Vol. 3 Sheet Silicates. Longmans, London.Google Scholar
Francis, G. H., 1955. Zoned Hydrothermal Bodies in the Serpentinite Mass of Glen Urquhart (Inverness-shire). Geol. Mag., 92, 433–447.CrossRefGoogle Scholar
Francis, G. H., 1956. The Serpentinite Mass in Glen Urquhart, Inverness-shire, Scotland. Amer. Jour. Sci., 254, 201–226.CrossRefGoogle Scholar
Fyfe, W. S., 1962. On the relative stability of Talc, Anthophyllite, and Enstatite. Amer. Jour. Sci., 260, 460–466.CrossRefGoogle Scholar
Fyfe, W. S., 1960, The Stratigraphical Evolution of the Midland Valley. Trans. geol. Soc. Glasgow, 24, 32–107.Google Scholar
Fyfe, W. S., and Oswald, D. H., 1957. The Carboniferous Rocks of the Donegal Syncline. Quart. J. geol. Soc. Lond., 113, 137–179.Google Scholar
Hardman, E. T., 1883. On the Metamorphic Rocks of Co's Sligo and Leitrim, etc., J. roy. geol. Soc. Ireland, 6, p. 172.Google Scholar
Hess, H. H., 1933. The problem of serpentinization and the origin of certain chrysotile asbestos, talc, and soapstone deposits. Econ. Geol., 28, 634–657.CrossRefGoogle Scholar
Hess, H. H., 1960. The Stillwater Igneous Complex. Mem. geol. Soc. Amer., 80.Google Scholar
Kilroe, J. R., 1885. Explanatory Memoir to Sheet 55. Mem. geol. Surv. Ireland.Google Scholar
Kulp, J. L., and Brobst, D. A., 1954. Notes on the Dunite and the Geochemistry of the Vermiculite at the Day Book Dunite deposits, Yancey County, North Carolina. Econ. Geol., 49, 211–223.CrossRefGoogle Scholar
Larsen, E. S., 1928. A Hydrothermal Origin of Corundum and Albitite bodies. Econ. Geol., 23, 398–433.CrossRefGoogle Scholar
Oswald, D. H., 1955. The Carboniferous Rocks between the Ox Mountains and Donegal Bay. Quart. J. geol. Soc. Lond., 111, 167–183.CrossRefGoogle Scholar
Randall, B. A. O. R., 1960. Sagvandites of Lyngen, Troms, North Norway. Rept. Internat. geol. Cong. Norden, Pt. 8., 443–451.Google Scholar
Swineford, Ada, et al., 1963. Clay and Clay Minerals. Pergamon Press.Google Scholar
Varley, E. R., 1952. Vermiculite. Col. geol. Surv. Min. Res. Divn.Google Scholar
Wilkinson, J. F. G., 1953. Some aspects of Alpine-type Serpentinites of Queensland. Geol. Mag., 90, 305–321.CrossRefGoogle Scholar
Wynne, A. B., 1885. Explanatory Memoir to Sheets 42 and 43. Mem. geol. Surv. Ireland.Google Scholar