Effect of water and stress on the lattice-preferred orientation of olivine

By H. Jung, I. Katayama, Zhenting Jiang, T. Hiraga, S. Karato. 2006

376 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/9e9caa5160e9d0d6df33f37fde1a76cb711df13a

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In Geophysics

Citations in the corpus

Upper mantle seismic anisotropy resulting from pressure-induced slip transition in olivine (2009, background): “that at high fugacity of H 2 O, the easiest slip direction in olivine changes from [100] to [001] and several different CPOs can be produced in the laborator”
Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, background): “Studies by Katayama et al. (2004), Jung et al. (2006), and Katayama and Karato (2006) mapped out the occurrence of five different olivine fabric types (the original A-type plus B-, C-, D-, and E-types).”
Low-temperature, high-stress deformation of olivine under water-saturated conditions (2008, background): “The IR spect a a r t ( f i m c 3 t a o o h r t F F T w t r c d ( e h t l u s t o b w t b L w t s s c t a w e o s t s e ε ra of the hot-pressed starting material and the wet single crystal (Jung et al., 2006) re shown for comparison.”
A new analysis of experimental data on olivine rheology (2008, methodology): “If this condition Figure 3. Pressure and temperature conditions for the four experimental studies compiled for this study: KPF86 [Karato et al., 1986] (circle), HK95 [Hirth and Kohlstedt, 1995a] (triangle), MK00 [Mei and Kohlstedt, 2000a, 2000b] (square), and J06 [ Jung et al., 2006 ] (star).”
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).”
Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (2008, methodology): “For each LPO, the corresponding dominant slip systems have been identified using the inverse pole figures ( Jung et al. 2006).”
Mantle dynamics and seismic anisotropy (2010, background): “…on the relationship between deformation and LPO come mainly from laboratory experiments (e.g., Zhang and Karato, 1995; Bystricky et al., 2000; Jung et al., 2006) and, for the uppermantle, from the petrographic examination of mantle-derived rocks (e.g., Nicolas et al., 1971; Ben Ismaïl and…”
Organized melt, seismic anisotropy, and plate boundary lubrication (2010, background): “First, experiments exploring effects of water and elevated stress have mapped out regimes of different LPOs, some characterized by nonparallelism between shear direction and seismic fast direction, [e.g., Jung et al., 2006].”