The responses of the four main substitution mechanisms of H in olivine to H2O activity at 1050 °C and 3 GPa-Reference-Cited by-同舟云学术

The responses of the four main substitution mechanisms of H in olivine to H2O activity at 1050 °C and 3 GPa

Published:2017-05-09 Issue:1 Volume:4 Page:
ISSN:2197-4284
Container-title:Progress in Earth and Planetary Science
language:en
Short-container-title:Prog. in Earth and Planet. Sci.

Author:

Tollan Peter M. E.,Smith Rachel,O’Neill Hugh St.C.,Hermann Jörg

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1186/s40645-017-0128-7.pdf

Reference63 articles.

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3. Bai Q, Kohlstedt DL (1993) Effects of chemical environment on the solubility and incorporation mechanism for hydrogen in olivine. Phys Chem Miner 19:460–471

4. Balan E, Ingrin J, Delattre S, Kovács I, Blanchard M (2011) Theoretical infrared spectrum of OH-defects in forsterite. Eur J Mineral 23(3):285–292

5. Bali E, Bolfan-Casanova N, Koga KT (2008) Pressure and temperature dependence of H solubility in forsterite: an implication to water activity in the Earth interior. Earth Planet Sci Lett 268(3–4):354–363

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