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III.—On a Case in which various massive Crystalline Rocks including Soda-Granite, Quartz-Diorite, Norite, Horn-blendite, Pyroxenite, and different Chrysolitic Rocks, were made through Metamorphic Agencies in one Metamorphic Process

Published online by Cambridge University Press:  01 May 2009

D. James Dana
D. James Dana
Affiliation:
For. Memb. Geol. Soc. Lond., of Yale College, New Haven, Ct., U.S.A.
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Extract

The extent of these bands, their number, uniformity of direction and apparently of dip, and the identity of the material constituting them with beds of the schist, especially the more northern, are such as to warrant the following section (Fig. 15).

Type
Original Articles
Information
Geological Magazine , Volume 8 , Issue 4 , April 1881 , pp. 162 - 171
Copyright
Copyright © Cambridge University Press 1881

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References

page 162 note 1 Reports of Progress, Geol. Survey of Canada, 1875–6, p. 266; 1876–7, p. 457; 1877–8, p. 175, B.

page 162 note 2 For additional information on the Tertiary rocks of the interior, see the following Reports of Progress, 1871–2, p. 56; 1875–6, pp. 70 and 225; 1876–7, pp. 75 and 112, B.