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An Alternative to the ‘Clastic Trap’ Interpretation of Oolitic Ironstone Facies

Published online by Cambridge University Press:  01 May 2009

M. Brookfield
Affiliation:
Dept. of Soil ScienceUniversity of GuelphOntario
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Abstract

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Type
Correspondence
Copyright
Copyright © Cambridge University Press 1972

References

Brookfield, M. The palaeoenvironment of the Abbotsbury Ironstone (Upper Jurassic, Dorset). Palaeontology (In press).Google Scholar
Carozzi, A. 1960. Microscopic Sedimentary Petrography. J. Wiley and Sons, New York, 485 pp.Google Scholar
Hallam, A. 1963. Observations on the palaeoecology and ammonite sequence of the Frodingham Ironstone (Lower Jurassic). Palaeontology 6, 554–74.Google Scholar
Hunter, R. E. 1970. Facies of iron sedimentation in the Clinton Group. In Fisher, G. W., Pettijohn, F. J. & Weaver, K. N. (Eds): Studies of Appalachian Geology: Central & Southern. Interscience, New York, 460 pp., p. 101121.Google Scholar
Schäfer, W. 1962. Aktuo-Paläontologie nach Studien in der Nordsee. Kramer, W., Frankfurt, , 666 pp.Google Scholar
Schellmann, W. 1969. Die Bildungsbedingungen sedimentärer Chamosit- und Hämatit-Eisenerze am Beispeil der Lagerstätte Echte. Neves Jb. Miner. Abh. 111, 131.Google Scholar
Winkelmolen, A. M. 1971. Rollability, a functional shape property of sand grains. Jour. Sed. Petrology 41, 703714.Google Scholar