Published online by Cambridge University Press: 01 May 2009
Professor Reynolds has recently described from one of the Arnold Quarries, Chipping Sodbury, a section in which several beds of the Carboniferous Limestone were seen individually to be thrust over, or underthrust by, Rhaetic deposits (Text-fig. 2).1 No decision was made as to the origin of this structure.
1 Geol. Mag., LXXV, 1938, pp. 97–100. The two text-figures are reproduced here by permission of Professor Reynolds.Google Scholar
1 Nevin, C. M., The Principles of Structural Geology, fig. xxxii, p. 50, 1936.Google Scholar