Characteristic features of x-ray diffraction on natural titanomagnetites after their spinodal decomposition-Reference-Cited by-同舟云学术

Characteristic features of x-ray diffraction on natural titanomagnetites after their spinodal decomposition

Published:2006-12 Issue:12 Volume:42 Page:1038-1043
ISSN:1069-3513
Container-title:Izvestiya, Physics of the Solid Earth
language:en
Short-container-title:Izv., Phys. Solid Earth

Author:

Gapeev A. K.,Gribov S. K.

Publisher

Pleiades Publishing Ltd

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

http://link.springer.com/content/pdf/10.1134/S106935130612007X.pdf

Reference18 articles.

1. T. G. Artemova and A. K. Gapeev, “On the Decomposition of Solid Solutions in the Magnetite-Ulvospinel System,” Izv. Akad. Nauk SSSR, Ser. Fiz. Zemli, No. 12, 82–87 (1988).

2. E. Z. Basta, “Natural and Synthetic Titanomagnetites (the System Fe3O4-Fe2TiO4-FeTiO3),” Neues Jahrb. Mineral 94, 1017–1048 (1960).

3. A. Guinier, Heterogeneous Metallic Solid Solutions (New York, 1959; IL, Moscow, 1962) [in Russian].

4. N. Kawai, “Subsolidus Phase Relation in Titanomagnetite and Its Significance in Rock-Magnetism,” Proc. 20th Int. Geol. Congr. A (Tokyo, 1956a), Vol. 11, pp. 103–120.

5. N. Kawai, “Exsolution of Titanomagnetites and Its Effect on Rock-Magnetism,” Proc. Jap. Acad. 32, 464–468 (1956b).

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