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Lattice-like inclusions in Calcite from North Burgess, Ontario
Published online by Cambridge University Press: 14 March 2018
Extract
The pale celestite-blue calcite which occurs on the eastern half of Lot 13, Range V, of North Burgess township, Lanark county, Ontario, contains very remarkable lattice-like inclusions of a hydrous magnesium silicate.
The calcite forms crystalline masses belonging to the Grenville series, which has a very extensive areal development in certain parts of Ontario. The texture varies from medium to very coarse, in which the individual cleavage-rhombs of calcite measure one inch or more in diameter. Repeated twinning on e (0112) or (101) is almost invariably exhibited, and is especially pronounced in the more coarsely crystallized varietiea Both the twinning and the crystalline character are results of the very intense metamorphism to which this Archaean limestone has been subjected.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 18 , Issue 85 , August 1918 , pp. 252 - 258
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1918
References
page 254 note 1 These were studied by Sir David Brewster in 1844, and described in greater detail by G. Rose, Über die im Kalkspath vorkommenden hohlen Canäle. Abhandl. Akad. Berlin, for 1868, 1869, 57-79.
page 257 note 1 Adams, F. D. and Barlow, A. E., Geology of the Haliburton and Bancroft areas, Province of Ontario. Geological Survey of Canada, Memoir No. 6, 1910, p. 213CrossRefGoogle Scholar.