Lattice preferred orientation in CaIrO3 perovskite and post-perovskite formed by plastic deformation under pressure-Reference-Cited by-同舟云学术

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Lattice preferred orientation in CaIrO3 perovskite and post-perovskite formed by plastic deformation under pressure

Published:2007-08-31 Issue:9 Volume:34 Page:679-686
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Niwa Ken,Yagi Takehiko,Ohgushi Kenya,Merkel Sébastien,Miyajima Nobuyoshi,Kikegawa Takumi

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-007-0182-6.pdf

Reference25 articles.

1. Carrez P, Ferre D, Cordier P (2007) Implications for plastic flow in the deep mantle from modeling dislocations in MgSiO3 minerals. Nature 446:68–70

2. Hammersley AP (1997) Fit2D: an introduction and overview. ESRF97HA02T, ESRF Grenoble, France

3. Hirose K, Fujita Y (2005) Clapeyron slope of the post-perovskite phase transition in CaIrO3. Geophys Res Lett 32:L13313. doi: 10.1029/2005GL023219

4. Hirose K, Kawamura K, Ohishi Y, Tateno S, Sata N (2005) Stability and equation of state of MgGeO3 post-perovskite phase. Am Mineral 90:262–265

5. Iitaka T, Hirose K, Kawamura K, Murakami M (2004) The elasticity of the MgSiO3 post-perovskite phase in the Earth’s lowermost mantle. Nature 430:442–445

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