Iron content of synthetic phlogopite as a function of growth rate-Reference-Cited by-同舟云学术

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Iron content of synthetic phlogopite as a function of growth rate

Published:1977-11 Issue:1 Volume:37 Page:150-153
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Baronnet A.,Velde B.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference7 articles.

1. Thermodynamic Theory of Affinity;De Donder,1936

2. The growth of crystals and the equilibrium structure of their surfaces;Burton;Philos. Trans. R. Soc. Lond.,1951

3. Solubilitéet croissance hydrothermales, caractérisation par topographic X, de phlogopite et muscovite;Corny,1975

4. Stability of biotite: experiment, theory and application;Wones;Am. Mineral.,1965

5. Determination of the equilibrium constant and the enthalpy of reaction for the Mg2+-Fe2+ exchange between biotite and a salt solution;Schulien;Fortschr. Mineral.,1975

Cited by 4 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Hydrothermal growth of OH-phlogopite single crystals;Journal of Crystal Growth;1989-06

2. The role of transition element adsorption on growth kinetics of the phlogopite mica;Chemical Geology;1988-08

3. Experimental metamorphic petrology;Reviews of Geophysics;1979

4. Solubility of phlogopite in basic aqueous solutions under hydrothermal conditions;Journal of Crystal Growth;1978-03

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