Lowell Miyagi , ' ' AnisotropyDImplications for Post - Perovskite : 3 Slip Systems in MgSiO

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  • Lowell Miyagi
چکیده

. clicking here colleagues, clients, or customers by , you can order high-quality copies for your If you wish to distribute this article to others . here following the guidelines can be obtained by Permission to republish or repurpose articles or portions of articles (this information is current as of September 28, 2010 ): The following resources related to this article are available online at www.sciencemag.org http://www.sciencemag.org/cgi/content/full/329/5999/1639 version of this article at: including high-resolution figures, can be found in the online Updated information and services, http://www.sciencemag.org/cgi/content/full/329/5999/1639/DC1 can be found at: Supporting Online Material http://www.sciencemag.org/cgi/content/full/329/5999/1639#otherarticles , 8 of which can be accessed for free: cites 35 articles This article http://www.sciencemag.org/cgi/collection/geochem_phys Geochemistry, Geophysics : subject collections This article appears in the following

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Miyagi , ' ' AnisotropyDImplications for Post - Perovskite : 3 Slip Systems in MgSiO

. clicking here colleagues, clients, or customers by , you can order high-quality copies for your If you wish to distribute this article to others . here following the guidelines can be obtained by Permission to republish or repurpose articles or portions of articles (this information is current as of September 23, 2010 ): The following resources related to this article are available online at ...

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Shear response of Fe-bearing MgSiO3 post-perovskite at lower mantle pressures

We investigate the shear response of possible slip systems activated in pure and Fe-bearing MgSiO(3) post-perovskite (PPv) through ab initio generalized stacking fault (GSF) energy calculations. Here we show that the [100](001) slip system has the easiest response to plastic shear among ten possible slip systems investigated. Incorporation of Fe(2+) decreases the strength of all slip systems bu...

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Plastic deformation of MgGeO3 post-perovskite at lower mantle pressures.

Polycrystalline MgGeO3 post-perovskite was plastically deformed in the diamond anvil cell between 104 and 130 gigapascals confining pressure and ambient temperature. In contrast with phenomenological considerations suggesting (010) as a slip plane, lattice planes near (100) became aligned perpendicular to the compression direction, suggesting that slip on (100) or (110) dominated plastic deform...

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The enigma of post-perovskite anisotropy: deformation versus transformation textures

The D00 region that lies just above the core mantle boundary exhibits complex anisotropy that this is likely due to preferred orientation (texturing) of the constituent minerals. (Mg,Fe)SiO3 post-perovskite is widely thought to be the major mineral phase of the D00. Texture development has been studied in various post-perovskite phases (MgSiO3, MgGeO3, and CaIrO3), and different results were ob...

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Deformation and texture development in CaIrO3 post-perovskite phase up to 6 GPa and 1300 K

At near ambient conditions, CaIrO3 is isostructural with the high-pressure polymorph MgSiO3 “post-perovskite” (pPv). MgSiO3 pPv is thought to be a major phase in the earth's lowermost mantle. CaIrO3 can thus serve as an analog for studying deformation of the pPv phase under conditions achievable with a multi-anvil deformation apparatus. Here we study the rheologic behavior of CaIrO3 pPv at a va...

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تاریخ انتشار 2010