Anisotropy of self-diffusion in forsterite grain boundaries derived from molecular dynamics simulations
Author:
Funder
Deutsche Forschungsgemeinschaft
Helmholtz-Gemeinschaft
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-016-1308-y.pdf
Reference51 articles.
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2. Adjaoud O, Steinle-Neumann G, Jahn S (2011) Transport properties of $$\text{Mg}_2\text{SiO}_4$$ Mg 2 SiO 4 liquid at high pressure: physical state of a magma ocean. Earth Planet Sci Lett 312:463–470. doi: 10.1016/j.epsl.2011.10.025
3. Adjaoud O, Marquardt K, Jahn S (2012) Atomic structures and energies of grain boundaries in $$\text{Mg}_2\text{SiO}_4$$ Mg 2 SiO 4 forsterite from atomistic modeling. Phys Chem Miner 39:749–760. doi: 10.1007/s00269-012-0529-5
4. Allen MP, Tildesley DJ (1989) Computer simulation of liquids. Clarendon Press, New York
5. Ammann MW, Brodholt JP, Dobson DP (2010) Simulating diffusion. Rev Miner Geochem 71(1):201–224. doi: 10.2138/rmg.2010.71.10
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