The Internal Structure of Fault Zones: I
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Kurz, W.; Imber, J.; Wibberley, C. A. J.; Holdsworth, R. E.; Collettini, C.
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Article
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2008
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Geological Society of London
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English
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Faults are primary focuses of both fluid migration and deformation in the upper crust. The recognition that faults are typically heterogeneous zones of deformed material, not simple discrete fractures, has fundamental implications for the way geoscientists predict fluid migration in fault zones, as