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The facing of faults

Published online by Cambridge University Press:  01 May 2009

Richard J. Lisle
Richard J. Lisle
Affiliation:
Department of Geology, University College, Swansea SA2 8PP, U.K.
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Abstract

It is proposed that the usage of the term structural facing be extended to include fault structures. Fault facing is defined as the direction in a fault plane which is at right angles to the trace of the bedding and is directed towards the younger beds. Certain types of faulted structures are found to have diagnostic patterns of facing variation.

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Type
Articles
Information
Geological Magazine , Volume 122 , Issue 3 , May 1985 , pp. 249 - 251
Copyright
Copyright © Cambridge University Press 1985

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References

Borradaile, G. J. 1976. Structural facing (Shackleton's Rule) and the Palaeozoic rocks of the Malaguide Complex near Velez Rubio, S.E. Spain. Proceedings. Koninklijke nederlandse akademie van wetenschappen B 79, 330–6.Google Scholar
Boyer, S. E. & Elliott, D. 1982. Thrust systems. Bulletin of the American Association of Petroleum Geologists 66, 1196–1230.Google Scholar
Butler, R. W. H. 1982. The terminology of structures in thrust belts. Journal of Structural Geology 4, 239–46.CrossRefGoogle Scholar
Coward, M. P. 1982. Surge zones in the Moine thrust zone of NW Scotland. Journal of Structural Geology 4, 247–56.CrossRefGoogle Scholar
Coward, M. P. & McClay, K. R. 1983. Thrust tectonics of South Devon. Journal of the Geological Society of London 140, 215–28.Google Scholar
Cummins, W. A. & Shackleton, R. M. 1955. The Ben Lui Recumbent Syncline (S.W. Highlands). Geological Magazine 92, 353–63.CrossRefGoogle Scholar
Dahlstrom, C. D. A. 1970. Structural geology in the eastern margin of the Canadian Rocky Mountains. Bulletin of Canadian Petroleum Geology 18, 332–406.Google Scholar
De Wit, M. J. 1982. Gliding and overthrust nappe tectonics in the Barberton Greenstone Belt. Journal of Structural Geology 4, 117–36.Google Scholar
Elliott, D. & Johnson, M. R. W. 1980. Structural evolution in the northern part of the Moine Thrust Belt, N.W. Scotland. Transactions of the Royal Society of Edinburgh: Earth Science 71, 69–96.Google Scholar
Harris, A. L. 1962. Dalradian geology of the Highland Border near Callander. Bulletin of the Geological Survey of Great Britain 19, 1–15.Google Scholar
Laing, W. P. 1977. Structural interpretation of drill core from folded and cleaved rocks. Economic Geology 72, 671–85.Google Scholar
Laubscher, H. P. 1977. An intriguing example of a folded thrust in the Jura. Eclogae Geologicae Helvetiae 70, 97–104.Google Scholar
Shackleton, R. M. 1958. Downward-facing structures of the Highland Border. Quarterly Journal of the Geological Society of London 113, 361–92.Google Scholar
Wood, B. L. 1978. The Otago Schist Megaculmination. Its possible origins and tectonic significance in the Rangitata Orogen of New Zealand. Tectonophysics 47, 339–68.Google Scholar