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The structural formula of a hydrous amphibole

  • G. D. Nicholls (a1) and J. Zussman (a1)
Abstract

The majority of amphiboles conform to the general structural formula X2-3Y5Z8O22(OH,F,Cl)2, where X = Na, K, Ca, Y - Mg, Fe″, Mn, A1, Fe‴, Ti, and Z = Si, A1 or Ti. Two X ions occupy the positions filled by Ca in the ideal tremolite structure; the additional X ions are assumed to occur in the 'A' sites which are vacant in tremolite.

For the amphiboles, therefore, the method most commonly adopted for deriving a formula from a chemical analysis is to assume that a total of 24 anions is present in the formula unit.

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References
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Buddington, (A.F.) and Leonaid, (B.F.), 1953. Amer. Min., vol. 38, p. 891. [M.A. 12-374.]
Hey, (M.H.), 1939. Min. Mag., vol. 25, p. 402.
Hey, (M.H.), 1954. Min. Mag., vol. 30, p. 481.
Hutton, (C.O.), 1940. Mem. Geol. Surv. New Zealand, no. 5, p. 15.
Hutton, (C.O.), 1943. Trans. Roy. Soc. New Zealand, vol. 73, p. 174. [M.A. 9-61,]
Mcconnell, (D.), 1950. Amer. Min., vol. 35, p. 166. [M.A. 11-220.]
Mcconnell, (D.), 1951. Clay Min. Bull., vol. 1, p. 179.
Warren, (B.E.), 1930. Zeits. Krist., vol. 72, p. 493. [M.A. 4-278.]
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Mineralogical Magazine
  • ISSN: 1876-1968
  • EISSN: 2515-821X
  • URL: /core/journals/mineralogical-magazine
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