Rheology of mixed deformation mechanisms and mineral phase assemblages. (December 2019)

• Record Type: Journal Article
• Authors: Hobbs, Bruce E.; Ord, Alison; Ulrich, Stanislav; Schulmann, Karel
• Is Part Of: Journal of structural geology. Volume 129(2019)
• Publication Date: 2019-12
• Subjects: Thermodynamic mixing relations -- Mixed deformation mechanisms -- Polymineralic aggregates -- Rachinger grain boundary sliding -- Topology of microstructure -- Grain size distributions.; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2019.103891
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: This paper examines the rheological behaviour of power law viscous materials arising from mixtures of deformation mechanisms and/or different mineral assemblages. The mixing relation is based on classical thermodynamics mixing relations where the enthalpy of the mixture is the sum of the molar volume proportions of the individual molar enthalpies; this is equivalent to the 1887 Arrhenius mixing relation for Newtonian viscosities. We compare this mixing relation to viscosities obtained from finite element simulations of deforming mixed mineral phases and from experimental results. The mixing relation helps understanding of apparent anomalies in experimental results for calcite and quartz. This then enables the construction of flow laws and of deformation mechanism maps for mixtures of deformation mechanisms and of mineral assemblages over a range of grain size distributions. The rheological implications for changes in the topology (such as anisotropy) of mineral arrangements, for mixtures of grain sizes, for the interpretation of experimental results and for geodynamic modelling are discussed. Highlights: Mixed deformation mechanisms and/or different mineral assemblages incorporated by a generalised mixing formulation. Mixing relation helps understanding of apparent anomalies in experimental results for calcite and quartz. Flow laws and deformation mechanism maps for mixtures of deformation mechanisms, mineral assemblages and grain-sizes enabled. Implications of microstructure and grain size distributions for experimental results and geodynamical modelling highlighted.