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January 01, 2017; Volume 439,Issue 1

The Geometry and Growth of Normal Faults

Editors: C. Childs, University College Dublin, Ireland
R. E. Holdsworth, University of Durham, UK
C. A.-L. Jackson, Imperial College, UK
T. Manzocchi, University College Dublin, Ireland
J. J. Walsh, University College Dublin, Ireland and
G. Yielding, Badley Geoscience Ltd, UK

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A normal fault zone in interbedded marls and lignites of Pliocene age, Mavropigi Mine, Ptolemais, northern Greece. The throw across the zone is 20 m. Photograph provided by the Fault Analysis Group.

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