Mg-Fe order-disorder in ferromagnesian silicates.

Research output: Chapter in Book/Report/Conference proceedingChapter

17 Citations (Scopus)

Abstract

The various contributions made in this field in the last two decades are critically reviewed. The authors present some of their results for the first time. The crystal-chemical details, which are necessary to understand the atomic forces governing Fe2+-Mg distribution in ferromagnesian silicates, as well as the experimental techniques commonly used to determine Fe2+-Mg distribution, are reviewed in Part I. Part II deals with the thermodynamics and kinetics of Fe2+-Mg order-disorder and their application to geological problems.-C.N.

Original languageEnglish (US)
Title of host publicationAdvances in physical geochemistry. Vol. 2
EditorsS.K. Saxena
PublisherSpringer-Verlag
Pages3-99
Number of pages97
StatePublished - 1982
Externally publishedYes

Fingerprint

crystal structure
silicate
thermodynamics
crystal
kinetics
distribution
chemical

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

Cite this

Ghose, S., & Ganguly, J. (1982). Mg-Fe order-disorder in ferromagnesian silicates. In S. K. Saxena (Ed.), Advances in physical geochemistry. Vol. 2 (pp. 3-99). Springer-Verlag.

Mg-Fe order-disorder in ferromagnesian silicates. / Ghose, S.; Ganguly, Jibamitra.

Advances in physical geochemistry. Vol. 2. ed. / S.K. Saxena. Springer-Verlag, 1982. p. 3-99.

Research output: Chapter in Book/Report/Conference proceedingChapter

Ghose, S & Ganguly, J 1982, Mg-Fe order-disorder in ferromagnesian silicates. in SK Saxena (ed.), Advances in physical geochemistry. Vol. 2. Springer-Verlag, pp. 3-99.
Ghose S, Ganguly J. Mg-Fe order-disorder in ferromagnesian silicates. In Saxena SK, editor, Advances in physical geochemistry. Vol. 2. Springer-Verlag. 1982. p. 3-99
Ghose, S. ; Ganguly, Jibamitra. / Mg-Fe order-disorder in ferromagnesian silicates. Advances in physical geochemistry. Vol. 2. editor / S.K. Saxena. Springer-Verlag, 1982. pp. 3-99
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