Published online by Cambridge University Press: 14 March 2018
Ganophyllite was first detected in the Benallt mine as small fibrous patches varying in colour from pale pink to brown, in the thin vein cutting ore in the Ty Canol incline from which the manganese-rich chlorite, pennantite, was described. These were identified by X-ray photographs. It had previously been found at the neighbouring Nant mine by Sir Arthur Russell in 1911.
page 343 note 1 Smith, W. Campbell, Bannister, F. A., and Hey, M. H., Min. Mag., 1946, vol. 27, p. 218.CrossRefGoogle Scholar
page 343 note 2 Russell, A., Min. Mag., 1946, vol. 27, p. 234 Google Scholar
page 343 note 3 A specimen obtained earlier and given me by Mr. Wills had flakes up to 4 mm. across, but it is not known from which part of the mine this was obtained. The ganophyllite is associated with white calcite which fluoresces pink in ultra-violet light.(B.M. 1945,108.)
page 344 note 1 A similar absorption scheme is recorded for a mineral taken to be a mica in one of the specimens carrying banalsite from Benallt described in 1944 (Min. Mag., vol. 27, p. 40).
page 344 note 2 Hamberg, A., Geol. För. Förh. Stockholm, 1890, vol. 12, pp. 586–598.CrossRefGoogle Scholar
page 344 note 3 Larsen, E. S. and Shannon, E. V., Ganophyllite from Franklin Furnace, New Jersey. Amer. Min., 1924, vol. 9, p. 239. [M.A. 3–216.]Google Scholar
page 350 note 1 Palache, C., Amer. Journ. Sci., 1910, ser. 4, vol. 29, p. 187.Google Scholar
page 351 note 1 Larsen, E. S. and Shannon, E. V., Amer. Min., 1922, vol. 7, p. 152. [M.A. 2–472.]Google Scholar
page 351 note 2 Ibid., 1924, vol. 9, pp. 238–240. [M.A. 3–216.]