Hostname: page-component-848d4c4894-8bljj Total loading time: 0 Render date: 2024-06-23T06:49:18.705Z Has data issue: false hasContentIssue false

A Pyroxene – Hornfels from the Basic Plutonic Complex, Co. Tyrone, Ireland

Published online by Cambridge University Press:  01 May 2009

N. S. Angus
Affiliation:
Department of Geology, The University, Hull

Summary

A basic augite-hypersthene-hornfels, which escaped a subsequent regional amphibolite facies metamorphism, is preserved adjacent to a gabbroic intrusion of the Basic Plutonic Complex. The hornfels and two dolerites have been analysed and their compositions compared with similar rocks from Duluth and Skye. It appears that Si, Na and K have been removed from the dolerites, and the resultant hornfels relatively enriched in Fe, Mg, Ti and Ca.

Type
Articles
Copyright
Copyright © Cambridge University Press 1970

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

Almond, D. C., 1964. Metamorphism of Tertiary lavas in Strathaird, Skye. Trans. roy. Soc. Edin., 65, 413434.Google Scholar
Angus, N. S., 1962. Ocellar Hybrids from the Tyrone Igneous Series, Ireland. Geol. Mag., 99, 926.CrossRefGoogle Scholar
Bailey, E. B., et al, 1924. The Tertiary and post-Tertiary geology of Mull, Loch Aline and Oban. Mem. geol. Surv. U.K.Google Scholar
Binns, R. A., 1965. The mineralogy of metamorphosed basic rocks from the Willyama complex, Broken Hill district, New South Wales. Part I. Hornblendes. Miner. Mag., 35, 306326.Google Scholar
Cobbing, E. J. 1964. In Summ. Prog. geol. Surv. Gt. Brit for 1963. 59.Google Scholar
Cobbing, E. J., Manning, P. I. & Griffith, A. E., 1965. Ordovician – Dalradian Unconformity in Tyrone. Nature, Lond. 206, 11321135.CrossRefGoogle Scholar
Engel, A. E. J., & Engel, C. G., 1962. Progressive metamorphism of amphibolite, northwest Adirondack Mountains, New York. Bull. geol. Soc. Am. Petrologic Studies (Buddington Volume), 3782.Google Scholar
Evans, B. W., 1964. Fractionation of elements in the pelitic hornfelses of the Cashel – Lough Wheelaun intrusion, Connemara, Eire. Geochim. Cosmochim. Acta. 28, 127156.CrossRefGoogle Scholar
Harker, A., 1950. Metamorphism. 3rd ed. Methuen, London.Google Scholar
Hartley, J. J., 1933. The Geology of North-Eastern Tyrone and the adjacent parts of County Londonderry. Proc R. Irish Acad., 41B, 218285.Google Scholar
Leake, B. E. & Skirrow, G., 1960. The pelitic homfelses of the Cashel – Lough Wheelaun intrusion, Co. Galway, Eire. J. Geol., 68, 2340.CrossRefGoogle Scholar
Norrish, K., & Hutton, J. T., 1969. An accurate X-ray spectrographic method for the analysis of a wide range of geological samples. Geochim. cosmochim. Acta, 33, 431453.CrossRefGoogle Scholar
Ramberg, H., 1948. Titanic iron ore formed by dissociation of silicates in granulite facies. Econ. Geol., 43, 553570.CrossRefGoogle Scholar
Riley, J. P., 1958a. The rapid analysis of silicate rocks and minerals. Anal. Chim. Acta, 19, 413428.CrossRefGoogle Scholar
Riley, J. P., 1958b. Simultaneous determination of water and carbon dioxide in rocks and minerals. Analyst, 83, 4249.CrossRefGoogle Scholar
Taylor, R. B., 1964. Geology of the Duluth Gabbro Complex near Duluth, Minnesota. Bull. Minn. geol. Surv. 44, 63 pp.Google Scholar