No CrossRef data available.
Published online by Cambridge University Press: 01 May 2009
Some repetition may be avoided in this note by roughly grouping the specimens, which have been forwarded to me by Dr. Callaway, as (A) Felsitic Rocks, or those resembling felstones; (B) Granitoid and Gneissic Rocks; and (C) Dioritic Rocks. The numbers attached correspond with the reference-numbers in Dr. Callaway's paper. I may mention that in examining the slides I was ignorant of their bearing on the views propounded by the author, and, in some cases, of the exact locality of the specimens.
page 125 note 1 Described by myself, Geol. Mag. 1877, 12. II. Vol. IV. p. 508.Google Scholar
page 126 note 1 Produced by crushing or strain: not uncommon near faults.
page 126 note 2 Quart. Journ. Geol. Soc. 1879, vol. xxxv. p. 322.Google Scholar