Hostname: page-component-78c5997874-8bhkd Total loading time: 0 Render date: 2024-11-10T11:10:05.815Z Has data issue: false hasContentIssue false
  • English
  • Français

Autometasomatic gneisses of the Currywongaun-Doughruagh syntectonic intrusion, Connemara Ireland

Published online by Cambridge University Press:  05 July 2018

N. S. Angus  and
R. Kanaris-Sotiriou
N. S. Angus
Affiliation:
Department of Geology, The University, Hull HU6 7RX
R. Kanaris-Sotiriou
Affiliation:
Department of Geology, The University, Sheffield S1 3JD
Get access Rights & Permissions [Opens in a new window]

Abstract

The Currywongaun and Doughruagh masses of northern Connemara represent a section through a syntectonic, partially layered intrusion formed of ultrabasic cumulates all having plagioclase of around An94. Differentiation and contamination of the magma from which these cumulates were precipitated ultimately produced an acid residuum which was responsible for the hydrous metasomatism of the earlier formed ultrabasic rocks resulting in the extensive formation of quartz-amphibole-anorthite gneisses in the petrogenetically ‘upper’ parts of the intrusion. Coexisting Ca-rich and Ca-poor amphiboles in the gneisses are interpreted as ‘frozen’ reaction intermediates that were in local equilibrium. The bulk-rock chemical data presented confirm that the compositions of the quartz-rich gneisses can be attributed almost entirely to the addition of Si to the ultrabasic rocks, coupled with the removal of Mg and Ca. The data also suggest that Zr, which reaches around 1000 ppm in some of the gneisses, may have been ‘mobile’ under these conditions of hydrothermal metasomatism.

Type
Research Article
Information
Mineralogical Magazine , Volume 46 , Issue 341 , December 1982 , pp. 411 - 420
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1982

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

Carswell, D. A., Curtis, C. D., and Kanaris-Sotiriou, R. (1974) J. Petrol. 15, 381–402 [MA 75-1595].CrossRefGoogle Scholar
Choudhuri, A. (1970) Mineral. Mag. 37, 923–28 [MA 71-693].CrossRefGoogle Scholar
Kanaris-Sotiriou, R., and Angus, N. S. (1976) J. Geol. Soc. Lond. 132, 485–508 [MA 77-914].CrossRefGoogle Scholar
Kanaris-Sotiriou, R., and Angus, N. S. (1979) Mineral. Mag. 43, 473–8 [MA 80-2521].CrossRefGoogle Scholar
Kisch, H. J., and Warnaars, F. W. (1969) Contrib. Mineral. Petrol. 24, 245–67 [MA 70-2526].CrossRefGoogle Scholar
Leake, B. E. (1969) Q. J. Geol. Soc. Lond. 125, 219–76 [MA 70-2814].CrossRefGoogle Scholar
Leake, B. E. (1970) In Mechanism of igneous intrusion. Newall, G., and Rast, N. (eds.), Spec. Publ. Geol. J. 2, 103–22 [MA 70-3508].Google Scholar
Leake, B. E. (1978) Mineral. Mag. 42, 533–63 [MA 791600].CrossRefGoogle Scholar
Leake, B. E. (1980) Am. Mineral. 65, 26–36 [MA 81-0989].Google Scholar
Livingstone, A., Frost, M. T., and Suddaby, P. (1973) Livingl. Mag. 39, 464–6 [MA 74-439].CrossRefGoogle Scholar
Luth, W. C., and Tuttle, O. F. (1969) Mere. Geol. Soc. Am. 115, 513–48 [MA 70-1655].Google Scholar
Morey, G. W., and Hesselgesser, H. M. (1951) Econ. Geol. 46, 821–35 [MA 12, 49].CrossRefGoogle Scholar
Sampson, G. A., and Fawcett, J. J., (1977) Can. Mineral. 15, 283–96 [MA 80-0703].Google Scholar
Stephenson, N. C. R, and Hensel, H. D. (1979) Ibid. 17, 11–23 CMA 80-0704].Google Scholar
Tuttle, O. F., and Bowen, N. L. (1958) Mere. Geol. Soc. Am. 74.Google Scholar
Vlasov, K. A. (1966) (ed.). Geochemistry and mineralogy of rare elements and genetic types of their deposits. 1 Geochemistry of rare elements. Israel Program for Scientific Translations, Jerusalem.Google Scholar