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Published online by Cambridge University Press: 14 March 2018
Inquiry into this feature was stimulated by a reasonable doubt concerning the reality of the immiscibility gap in the clinoenstatite-diopside series. The existence of this gap was first suspected by Sosman and Asklund, and the identity of the gap with the composition field of the hornblendes has recently been suggested by Kennedy, whose comparative study of hornblende and pyroxene composition engaged statistical methods applied in the first instance by Asklund.
page 362 note 1 Sosman, R. B., Minerals and rocks of the composition MgSiO3-CaSiO3-FeSiO3 . Journ. Washington Acad. Sci., 1911, vol. 1, pp. 54-58.Google Scholar
page 362 note 2 Asklund, Petrological studies in the neighbourkood of Stavsjö... ,Årsbok Sveriges Geol. Undersök., 1923, vol. 17, no. 6, pp. 75-88.
page 362 note 3 Kennedy, W. Q., The influence of chemical factors on the crystallization of hornblende in igneous rocks.Min. Mag., 1935, vol. 24, pp. 203-207.CrossRefGoogle Scholar
page 362 note 4 W. Q. Kennedy, loc. cit., p. 205, fig. 1.
page 363 note 1 Wiseman, J. D. H., Quart. Journ. Geol. Soc. London, 1934, vol. 90, pp. 354-417.CrossRefGoogle Scholar
page 363 note 2 Bowen, N. L., The evolution of the igneous rocks. 1928, p. 60.Google Scholar