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Journal of the Geological Society; 2000; v. 157; issue.6; p. 1261-1264
© 2000 Geological Society of London

Discussion on geometry and origin of a polygonal fault system

Journal, Vol. 157, 2000, 151–162

D. M. D. JAMES, J. J. WALSH, J. WATTERSON, A. NICOL, P. A. R. NELL & P. BRETAN

1 3 Finedon Hall, Finedon NN9 5NG, UK (e-mail: davidjoanjames{at}compuserve.com)
2 Fault Analysis Group, Department of Geology, University College Dublin, Belfield, Dublin 4, Ireland (e-mail: fault{at}fag.ucd.ie)
3 Fault Analysic Group, Liverpool University Marine Laboratory, Port Erin Isle of Man, IM9 6JA, UK
4 Institute of Geological and Nuclear Sciences, PO Box 30-368, Lower Hutt, New Zealand
5 Badley Earth Sciences Ltd, North Beck House, North Beck Lane, Hundleby, Lincs PE23 5NB, UK



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  		Fig. 1. Seismic sections in in-line (a) and cross-line (b) directions (locations as in GoWatterson et al. 2000, fig. 2) with interpreted faults and horizons (Cadna-owie, Ca; Coorikiana, Co; Mackunda, M). Vertical exaggeration is c. 2.4. Modified after GoWatterson et al. (2000, fig. 3).