Large-strain deformation and strain partitioning in polyphase rocks: Dislocation creep of olivine–magnesiowüstite aggregates |
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| Authors: | Misha Bystricky Florian Heidelbach Steve Mackwell |
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| Institution: | aGeologisches Institut, ETH Zürich, 8092 Zürich, Switzerland;bLaboratoire des Mécanismes et Transferts en Géologie, UMR 5563, Observatoire Midi-Pyrénées, Université Paul Sabatier, 31400 Toulouse, France;cBayerisches Geoinstitut, Universität Bayreuth, 95440 Bayreuth, Germany;dLunar and Planetary Institute, Houston, TX 77058, USA |
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| Abstract: | Aggregates composed of olivine and magnesiowüstite have been deformed to large strains at high pressure and temperature to investigate stress and strain partitioning, phase segregation and possible localization of deformation in a polyphase material. Samples with 20 vol.% of natural olivine and 80 vol.% of (Mg0.7Fe0.3)O were synthesized and deformed in a gas-medium torsion apparatus at temperatures of 1127 °C and 1250 °C, a confining pressure of 300 MPa and constant angular displacement rates equivalent to constant shear strain rates of 1–3.3 × 10− 4 s− 1. The samples deformed homogeneously to total shear strains of up to γ  15. During constant strain rate measurements the flow stress remained approximately stable at 1250 °C while it progressively decreased after the initial yield stress at the lower temperature. Mechanical data, microstructures and textures indicate that both phases were deforming in the dislocation creep regime. The weaker component, magnesiowüstite, controlled the rheological behavior of the bulk material and accommodated most of the strain. Deformation and dynamic recrystallization lead to grain refinement and to textures that were not previously observed in pure magnesiowüstite and may have developed due to the presence of the second phase. At 1127 °C, olivine grains behaved as semi-rigid inclusions rotating in a viscous matrix. At 1250 °C, some olivine grains remained largely undeformed while deformation and recrystallization of other grains oriented for a-slip on (010) resulted in a weak foliation and a texture typical for pure dry olivine aggregates. Both a-slip and c-slip on (010) were activated in olivine even though the nominal stresses were up to 2 orders of magnitude lower than those needed to activate these slip systems in pure olivine at the same conditions. |
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| Keywords: | Olivine Magnesiowü stite Deformation Rheology Polyphase Strain partitioning Large strain Torsion Recrystallization SPO CPO LPO |
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