A subsidiary fast-diffusing substitution mechanism of Al in forsterite investigated using diffusion experiments under controlled thermodynamic conditions-Reference-Cited by-同舟云学术

A subsidiary fast-diffusing substitution mechanism of Al in forsterite investigated using diffusion experiments under controlled thermodynamic conditions

Published:2017-06-05 Issue:7 Volume:172 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Zhukova Irina,O’Neill Hugh,Campbell Ian H.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/article/10.1007/s00410-017-1365-x/fulltext.html

Reference43 articles.

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3. Beattie P (1994) Systematics and energetics of trace-element partitioning between olivine and silicate melts—implications for the nature of mineral melt partitioning. Chem Geol 117:57–71

4. Berry AJ, Hermann J, O’Neill HSC, Foran GJ (2005) Fingerprinting the water site in mantle olivine. Geology 33:869–872

5. Berry AJ, O’Neill HSC, Hermann J, Scott DR (2007) The infrared signature of water associated with trivalent cations in olivine. Earth Planet Sci Lett 261:134–142

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