Different facies of deformation observed in cores of limestone lithology: a: compaction related stylolithes and associated extension calcite veins in mudstones; b: in marly limestones; c: brecciated limestones in fault damage zone, note mudstones and clasts of calcite vein; d: intense deformation in fault core zone characterised by centimetre-scale extensional shear-zones (arrows) affecting both stylolitized limestones and veins; note the genetic relationship between bedding-parallel stylolites and sub-vertical calcite veins in the poorly deformed host limestone; e: hydraulic breccia sealed by calcite; note the late vertical fractures, partially cemented.