Modelling garnet-fluid partitioning in H2O-bearing systems: a preliminary statistical attempt to extend the crystal lattice-strain theory to hydrous systems-Reference-Cited by-同舟云学术

Modelling garnet-fluid partitioning in H2O-bearing systems: a preliminary statistical attempt to extend the crystal lattice-strain theory to hydrous systems

Published:2020-07-30 Issue:8 Volume:175 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Meltzer Amit^ORCID,Kessel Ronit

Funder

Israel Science Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00410-020-01719-8.pdf

Reference75 articles.

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2. Allegre C, Minster J (1978) Quantitative models of trace element behavior in magmatic processes. Earth Planet Sci Lett 38:1–25

3. Antignano A, Manning CE (2008) Rutile solubility in H2O, H2O–SiO2, and H2O–NaAlSi3O8 fluids at 0.7–2.0 GPa and 700–1000 C: implications for mobility of nominally insoluble elements. Chem Geol 255:283–293

4. Audétat A, Keppler H (2005) Solubility of rutile in subduction zone fluids, as determined by experiments in the hydrothermal diamond anvil cell. Earth Planet Sci Lett 232:393–402

5. Ayers JC, Dittmer SK, Layne GD (1997) Partitioning of elements between peridotite and H2O at 2.0–3.0 GPa and 900–1100 C, and application to models of subduction zone processes. Earth Planet Sci Lett 150:381–398

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