1Department for Geodynamics and Sedimentology, University
of Vienna, Althanstrasse 14, 1090 Vienna, Austria
2Natural History Museum, Burgring 7, 1010 Vienna,
3Department of Earth Sciences, University of New
Brunswick, 3 Bailey Dr, Fredericton, NB E3B 5A3, Canada
Received: 09 Aug 2015 – Discussion started: 18 Sep 2015
Abstract. Extreme strain localization occurred in the centre of the cross-cutting element of a flanking structure in almost pure calcite marbles from Syros, Greece. At the maximum displacement of 120 cm along the cross-cutting element, evidence of grain size sensitive deformation mechanisms can be found in the ultramylonitic marbles, which are characterized by (1) an extremely small grain size ( ∼ 3 µm), (2) grain boundary triple junctions with nearly 120° angles, (3) a weak crystallographic preferred orientation with very low texture index (J = 1.4), (4) a random misorientation angle distribution curve and (5) the presence of small cavities. Using transmission electron microscopy, a deformation sequence is observed comprising recrystallization dominantly by bulging, resulting in the development of the fine-grained ultramylonite followed by the development of a high dislocation density ( ∼ 1013 m−2) with ongoing deformation of the fine-grained ultramylonite. The arrangement of dislocations in the extremely fine-grain-sized calcite differs from microstructures created by classical dislocation creep mediated by combined glide and thermally activated climb. Instead, it exhibits extensive glide and dislocation networks characteristic of recovery accommodated by cross-slip and network-assisted dislocation movement without formation of idealized subgrain walls. The enabling of grain boundary sliding to dislocation activity is deemed central to initiating and sustaining strain softening and is argued to be an important strain localization process in calcite rocks, even at a high strain rate ( ∼ 10−9 s−1) and low temperature (300 °C).
Revised: 15 Feb 2016 – Accepted: 20 Feb 2016 – Published: 08 Mar 2016
Rogowitz, A., White, J. C., and Grasemann, B.: Strain localization in ultramylonitic marbles by simultaneous activation of dislocation motion and grain boundary sliding (Syros, Greece), Solid Earth, 7, 355-366, doi:10.5194/se-7-355-2016, 2016.