Bullock, Rachael J. and De Paola, Nicola and Holdsworth, Robert E. and Trabucho-Alexandre, João (2014) 'Lithological controls on the deformation mechanisms operating within carbonate-hosted faults during the seismic cycle.', Journal of structural geology., 58 . pp. 22-42.
A significant proportion of moderate-large earthquakes, plus aftershocks, nucleate within and propagate through upper-crustal carbonate-dominated sequences, where the effects of lithological variations on fault behaviour are poorly understood. The Gubbio fault is an active (1984, Ms = 5.2) normal fault in Italy, hosted in Mesozoic–Cenozoic limestones and interbedded marls. Fault core domains derived from limestone at the studied outcrop are characterised by fractures/hydrofractures and breccias and host a number of localised (<1.5 mm wide) principal slip zones (PSZs). The majority of displacement of up to 230 m is concentrated in these PSZs, which comprise cataclasites, gouges, and calcite veins. Degassing bubbles, ‘quenched’ calcite, and the transformation of smectite to illite, are also observed within PSZs, implying frictional heating and seismic slip. In contrast, marl-rich domains exhibit distributed shear planes bounding a continuous and pervasive foliation, defined by phyllosilicate-rich pressure-solution seams. Microstructures in the seams include folds/kinks of phyllosilicates and pressure shadows around clasts, consistent with aseismic fault creep. A model is proposed for the behaviour of lithologically complex carbonate-hosted faults during the seismic cycle, whereby limestone-dominated fault core domains behave in a predominantly seismic manner, whereas phyllosilicate-rich domains behave in a predominantly aseismic manner.
|Keywords:||Carbonate fault, Phyllosilicate, Fault zone heterogeneity, Seismic behaviour, Microstructure, Deformation mechanisms.|
|Full text:||(VoR) Version of Record|
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|Publisher Web site:||https://doi.org/10.1016/j.jsg.2013.10.008|
|Publisher statement:||This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. © 2013 The Authors. Published by Elsevier Ltd.|
|Date accepted:||20 October 2013|
|Date deposited:||17 February 2014|
|Date of first online publication:||02 November 2013|
|Date first made open access:||No date available|
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