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Journal of the Geological Society; 2008; v. 165; issue.2; p. 449-452;
DOI: 10.1144/0016-76492007-129
© 2008 Geological Society of London

Short Communication

Fabric anisotropy controls faulting in the continental crust

R.W.H. Butler1,4, C.E. Bond2, Z.K. Shipton2, R.R. Jones3 & M. Casey1

1 Institute of Geophysics and Tectonics, The University of Leeds, Leeds LS2 9JT, UK (e-mail: r.butler{at}see.leeds.ac.uk)
2 Department of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK
3 Geospatial Research Ltd, Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK
4 Present address: School of Geosciences, Meston Building, University of Aberdeen, Aberdeen AB24 3UE, UK (e-mail: rob.butler{at}abdn.ac.uk)

The influence of pre-existing structural anisotropy on faulting in the continents is best tested in recently exhumed crust (e.g. Nanga Parbat Massif, NW Himalayas), where earlier brittle structures have been annealed. The kinematics of young faults, formed in a single, continuing tectonic regime (NNW compression), are distinctly different, depending upon the orientation of the early ductile foliations around them. Faulting is subparallel and statistically simple where foliation is moderately dipping but highly complex where foliation is steeply dipping. Thus structural anisotropy does control faulting in the continental crust, a result with important implications for seismogenesis, fluid flow and basin evolution.