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Published online by Cambridge University Press: 01 May 2009
In the most westerly working of Peldar Tor Quarry, in the northwest district of Charnwood Forest, a basic dyke is intruded into the porphyroid. Professor T. G. Bonney1 briefly described the dyke in 1915. The intrusion shows a remarkable laminated margin, and the present paper is chiefly directed to a consideration of this feature.
page 170 note 1 Bonney, , Geol. Mag., 1915, p. 548.Google Scholar
page 170 note 2 Daly, , Igneous Rocks, New York, 1914, p. 25.Google Scholar
page 171 note 1 Iddings, , Igneous Rocks vol. ii, New York, 1913, p. 142, No. 2.Google Scholar
page 171 note 2 Bonney, , & Hill, , Quart. Journ. Geol. Soc., vol. xxxvi, p. 342, 1880.Google Scholar