Simple shear deformation of olivine aggregates

By Shuqing Zhang, S. Karato, J. Gerald, U. Faul, Yi Zhou. 2000

189 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/bd941ea9dddcca707454afb8e48cd5f408119532

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

1. S. Karato
2. Y. Ricard
3. I. Katayama
4. N. Ribe
5. É. Kaminski
6. J. Browaeys
7. D. Bercovici
8. H. Jung

Citations in the corpus

• Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (2008, background): “(a) Axial compression is converted to nearly simple shear deformation of the bulk of a sample in this assembly, with a small additional component of compressional deformation (see Zhang & Karato 1995, Zhang et al. 2000).”
• A kinematic model for recrystallization and texture development in olivine polycrystals (2001, methodology): “The LPO of newly recrystallized grains is more complex, as they are either aligned with the shear direction, or perpendicular to the maximum compressional stress [33].”
• Effect of water and stress on the lattice-preferred orientation of olivine (2006, result): “First of all, previous experimental studies were conducted in samples with relatively small water content (Nicolas et al., 1973; Zhang and Karato, 1995; Zhang et al., 2000; Bystricky et al., 2000; Lee et al., 2002).”
• A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization (2011, background): “Other experimental piezometers have been proposed at different temperature and for olivine with different water contents (Post 1977; Karato et al. 1980; Ross et al. 1980; Van der Wal et al. 1993; Zhang et al. 2000; Jung & Karato 2001; Jung et al. 2006).”
• Low-temperature, high-stress deformation of olivine under water-saturated conditions (2008, background): “…in this paper, deformation experiments were erformed to large strains and deformation was likely at steadytate (quasi steady-state is achieved at shear strain of ∼0.2–0.4 F d v d Planetary Interiors 168 (2008) 125–133 nder wet conditions at similar T/Tm (Zhang et al., 2000; Jung et l., 2006)).”
• D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle (2004, background): “The comparison between the data of Bystricky et al. (2000) (complete LPO) and Zhang et al. (2000) (mainly relict grains) shows one common point and one difference.”
• Effects of pressure on high-temperature dislocation creep in olivine (2003, background): “Previous studies on olivine showed that, after the completion of dynamic recrystallization, the mechanical behaviour becomes nearly steady state (for example Zhang et al. (2000)).”
• Statistical properties of seismic anisotropy predicted by upper mantle geodynamic models (2006, unknown): “LPO and FSE Fast Axes [22] Figure 3 compares the spatial patterns of azimuthal anisotropy predicted at 200 km depth, from the FSE as a proxy and from best fitting, fast symmetry TI axes, as computed from the full C tensor based on the predicted LPO.”