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A New Structure in the Forest Marble of Oxford
Published online by Cambridge University Press: 01 May 2009
Abstract
An account is given of a new minor structural feature recently found in the Forest Marble of Bladon, Oxfordshire, resembling Pit and Mound structure, and various suggestions as to its mode of origin are discussed.
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References
REFERENCES
Arkell, W. J., 1933. New evidence on the Great Oolite Succession at Bladon, near Woodstock, Oxfordshire. Proc. Geol. Assoc., xliv, 177–183.CrossRefGoogle Scholar
Fenton, C. L., and Fenton, M. A., 1937. Belt Series of the North. Stratigraphy Sedimentation, Palaeontology. Bull. Geol. Soc. Amer., xlviii, 1941–8.Google Scholar
Kindle, E. M., 1916. Small Pit and Mound Structure developed during sedimentation. Geol. Mag., liii, 542–7.CrossRefGoogle Scholar
Lyell, C., 1851. On Fossil Rain-marks of the Recent, Triassic, and Carboniferous Periods. Quart. Journ. Geol. Soc., vii, 238.CrossRefGoogle Scholar
Madigan, C. T., 1928. Preliminary notes on new evidence as to the age of the formations on the North Coast of Kangaroo Island. Trans. Roy. Soc. S. Aust., lii, 210–216.Google Scholar
Schofield, R. K., and Keen, B. A., 1929. Rigidity in weak clay suspensions. Nature, cxxiii, 492–3.CrossRefGoogle Scholar
Woodward, H., 1910. On some supposed Pholas-borings from the shores of Birket el Qurûn, the Ancient Lake Moeris, of the Fayûm, Egypt. Geol. Mag., xlvii, 398–402.CrossRefGoogle Scholar