Note 393 — Chapter XLVI · TYPES OF STRUCTURE IN THE ACID ROCKS—BOSSES
Reading edition
I think it probable that some of the greenish portions of the granophyre along this part of the junction-line will be found to have had their structure and composition altered by having incorporated into their substance a proportion of the bedded basalts through which they have been disrupted.
[394] The dykes of granophyre in these basalts are referred to at p. 444.