Upper mantle seismic anisotropy resulting from pressure-induced slip transition in olivine
By H. Jung, W. Mo, H. Green. 2009
161 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/96c8f99e41c29db9d8f89b15a647854aa40b4698
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In Geophysics
- M. Long
- Thorsten W. Becker
- P. Silver
- Mark D. Behn
- Clinton P. Conrad
- G. Ekström
- B. Kustowski
- B. Steinberger
Citations in the corpus
- Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, background): “A recent study by Jung et al. (2009) on dry olivine reported a transition from A-type to B-type fabric at *3GPa, which corresponds to a depth of *90 km in the mantle.”
- Mantle dynamics and seismic anisotropy (2010, background): “…of deformation, including stress, temperature, and water content (e.g., Jung et al., 2006) and possibly pressure (e.g., Mainprice et al., 2005; Jung et al., 2009), although therehas been somedebate about the relative roles of pressure, stress, and water content in controlling LPO in some…”