Hostname: page-component-cd9895bd7-gbm5v Total loading time: 0 Render date: 2024-12-23T15:51:00.106Z Has data issue: false hasContentIssue false
  • English
  • Français

Chess-Board Albite from New Brunswick, Canada

Published online by Cambridge University Press:  01 May 2009

John Starkey
John Starkey
Affiliation:
The Jane Herdman Laboratories of Geology, The University of Liverpool.
Get access Rights & Permissions [Opens in a new window]

Abstract

Chess-board albite is described and theories on its origin outlined. A new occurrence from New Brunswick, Canada, is noted and certain features of the chess-board albite, discussed which fit the theory that it results from two processes, namely metasomatism of potash feldspar to soda feldspar, and deformation. This hypothesis is applied to British localities.

Type
Articles
Information
Geological Magazine , Volume 96 , Issue 2 , April 1959 , pp. 141 - 145
Copyright
Copyright © Cambridge University Press 1959

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

Anderson, O., 1928. The Genesis of some types of Feldspar from Granite Pegmatites. Norsk. Geol. Tidsskrift, x, 116–208.Google Scholar
Battey, M. H., 1955. Alkali Metasomatism and the Petrology of Some Keratohyres. Geol. Mag. xcii, 104–126.CrossRefGoogle Scholar
Becke, F., 1906. Zur Physiography der Gemengteile der Krystallinen Schiefer. Denk. Kias, Akad. der Wissenschaften, Mathe. Nat. Kl., xxv, 97–152.Google Scholar
Cox, A. H., 1915. The Geology of the District between Abereiddy and Abercastle, Pembrokeshire. Quart. Journ. Geol. Soc., lxxi, 273–342.CrossRefGoogle Scholar
Cummins, W. A., 1957. The Denbigh Grits; Wenlock Greywackes in Wales. Geol. Mag., xciv, 433–451.CrossRefGoogle Scholar
Emmons, R. C., 1953. Selected Petrogenic Relationships of Plagioclase. Geol. Soc. Amer., Mem. lii, 1–142.Google Scholar
Emmons, R. C., and Gates, R. M., 1943. Plagioclase Twinning. Bull. Geol. Soc. Amer., liv, 287–304.Google Scholar
Exner, C., 1949. Tektonik, Feldsparausbildung und deren gegenseitige Beziehungen in den ostlichen Hohen Tauern. Min. Pet. Mitt., xxx, 1, 197–284.Google Scholar
Gilluly, J., 1933. Replacement Origin of the Albite Granite Near Sparta, Oregen. U.S. Geol. Surv., Prof. Papers, clxxv, C, 65–81.Google Scholar
Grubenmann, U., and Niggli, P., 1924. Die Gesteinsmetamorphose, 1.Google Scholar
Hughes, E. W., 1917. On the Geology of the District from Cil-y-Coed to the St. Annes-Llanllyfni Ridge, Caernarvonshire. Geol. Mag., iv, 12–25.CrossRefGoogle Scholar
Niggli, P., 1954. Rocks and Mineral Deposits. (Trans. by Parker, R. L..)Google Scholar
Peach, B. N., 1911. The Geology of Knapdale, Jura and N. Kintyre. Mem. Geol. Surv. Scotland.Google Scholar
Tilley, C. E., 1919. The Petrology of the Granitic Mass of Cape Willoughby, Kangaroo Island, Part 1. Trans. and Proc. Roy Soc. S. Australia, xliii, 316–341.Google Scholar
Ussher, W. A. E., 1913. The Geology of Newton Abbot. Mem. Geol. Surv. England and Wales.Google Scholar