An Appinitic Facies Associated with Certain Granites in Jersey, Channel Islands
- 1 September 1955
- journal article
- Published by Geological Society of London in Quarterly Journal of the Geological Society
- Vol. 111 (1-4), 143-166
- https://doi.org/10.1144/gsl.jgs.1955.111.01-04.08
Abstract
The rocks here referred to as appinites form part of the essentially dioritic facies marginal to both the north-western and south-eastern complexes in Jersey. Mineralogically they are characterized by abundant long prismatic amphiboles, rich in titanium. Many of these contain cores of mica or felsic material, the nature and origin of which are discussed.Keywords
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