The Curie Point and the α–γ transition of iron to 53 Kbar — A reexamination-Reference-Cited by-同舟云学术

The Curie Point and the α–γ transition of iron to 53 Kbar — A reexamination

Published:1979 Issue:B2 Volume:84 Page:656
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Mirwald Peter W.,Kennedy George C.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v084/iB02/JB084iB02p00656/JB084iB02p00656.pdf

Reference9 articles.

1. The lattice expansion of iron;Basinski;Proc. Roy. Soc. Ser. A,1955

2. Detection of the α-γ iron phase transformation by differential thermal analysis;Claussen;Rev. Sci. Instrum.,1960

3. The structure of metals and alloys;Hume-Rothery,1962

4. U.S. Bur. Mines Bull.;Kelley,1960

5. A differential thermal analysis study of the high-temperature polymorphism of calcite at high pressures;Mirwald;Contrib. Mineral. Petrol.,1976

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