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  3. Deformation mechanisms in second-phase affected microstructures and their energy balance

Deformation mechanisms in second-phase affected microstructures and their energy balance

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DOI
10.7892/boris.73890
Publisher DOI
10.1016/j.jsg.2003.10.006
Abstract
Based on the relationship Zener parameter (Z=second-phase size/second-phase volume fraction) vs. calcite grain size (dg), second-phase controlled aggregates and microstructures that are weakly affected by second-phases are discriminated. The latter are characterized by large but constant grain sizes, high calcite grain boundary fractions and crystallographic preferred orientations (CPO), while calcite grain size and calcite grain boundary fraction decrease continuously and CPO weakens with decreasing Z in second-phase controlled microstructures. These observations suggest that second-phase controlled microstructures predominantly deform via granular flow because pinning of calcite grain boundaries reduces the efficiency of dynamic recrystallization favoring mass transfer processes and grain boundary sliding. In contrast, the balance of grain size reduction and growth by dynamic recrystallization maintains a steady state grain size in microstructures that are only weakly affected by second-phases promoting a predominance of dislocation creep. With increasing temperature, the relationship between Z and dg persists but the calcite grain size increases continuously. Based on microstructures, the energy of each modifying process is calculated and its relative contribution is compared with energies of the competing processes (surface energy, dragging energy, dynamic recrystallization energy). The steady state microstructures result from a temperature-dependent energy minimization procedure of the system.
Date Issued
2004
Publication Type
Article
Subject(s)
500 Science > 550 Earth sciences & geology
Language(s)
en
Author(s)
Herwegh, Marco  orcid-logo
Institut für Geologie  
Berger, Alfons  orcid-logo
Institut für Geologie  
Additional Credits
Institut für Geologie  
Journal
Journal of structural geology
Publisher
Pergamon
ISSN
0191-8141
Access(Rights)
restricted
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