Microstructural Evidence for Grain Size Sensitive Deformation Mechanisms in Naturally Deformed Peridotites

By J. Warren, Matthias H. Braun, G. Hirth, Dana S. Henry. 2002

354 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/63483da3770f6c7024d92c010d65398e77db028b

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In Geophysics

1. Y. Ricard
2. D. Bercovici
3. N. Dauphas
4. Jun Korenaga
5. S. Karato
6. M. Hirschmann
7. B. Kaus

Citations in the corpus

• Abyssal peridotites reveal the near-chondritic Fe isotopic composition of the Earth (2013, background): “Spinel Cr] and clinopyroxene trace element concentrations are from previous studies (Jaroslow et al., 1996; Stracke et al., 2011; Warren and Hirth, 2006; Warren et al., 2009).”
• Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning (2012, background): “…concentration of obstructing surfaces pins or constrains the mineral grains to ever smaller sizes, which forces the rheology to remain in diffusion creep (also experimentally inferred by Etheridge and Wilkie, 1979; Warren and Hirth, 2006; Mehl and Hirth, 2008), while also blocking grain growth.”