Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-26T00:24:48.658Z Has data issue: false hasContentIssue false

Some observations on the relationship between etch-pit form and structure in biotite

Published online by Cambridge University Press:  09 July 2018

J. A. Medina
Affiliation:
Departamento de Geología
M. Morante
Affiliation:
Departamento de Geología
S. Leguey
Affiliation:
Departamento de Geología
J. Tornero
Affiliation:
Departamento de Electroquímica, Facultad de Ciencias, Universidad Autónoma de Madrid, Cantoblanco, Madrid 34, Spain

Extract

The object of this study was to find a structural explanation for the corrosion figures produced in biotites having different chemical compositions and to apply this information to other di- or trioctahedral micas. The biotites investigated were used in earlier studies of epitaxial growth, so that previous knowledge of their surface behaviour was available. The biotites studied were from Evje, Norway (number 1), Guomum, Czechoslovakia (number 2), and Tanokami Yama, Japan (number 3). All were very dark in colour due to their high iron content.

Type
Notes
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1985

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bancroft, G.M. & Brown, J.R. (1975) A MÖssbauer study of co-existing hornblendes and biotites: quantitative Fe3+/Fe2+ ratios. Am. Miner. 60, 265272.Google Scholar
Desprairies, A. (1983) Relation entre le parametre b des smectites et leur contenue en fer et magnesium. Application a l'etude des sediments. Clay Miner. 18, 165175.CrossRefGoogle Scholar
Foster, M.D. (1960) Interpretation of the composition of trioctahedral micas. Prof. Pap. U.S. Geol. Surv. 354B, 1148.Google Scholar
Martin Ramos, J.D. & Rodriguez Gallego, M. (1980) Coexistencia de moscovitas 3T y 2M1 en gneises de la unidad de la Caldera (Cordillera Bética). Est. Geol. 36, 201204.Google Scholar
Radoslovitch, E.W. & Norrish, K. (1962) The cell dimensions and symmetry of layer lattice silicates. I. Some structural considerations. Am. Miner. 47, 599616.Google Scholar
Sanz, J. & Stone, W.E.E. (1979) NMR study of micas: II. Distribution of Fe2+, F- and OH- in the octahedral sheet of phlogopitcs. Am. Miner. 64, 119126.Google Scholar
Sanz, J. & Stone, W.E.E. (1983a) NMR study of minerals: III. The distribution of Mg2+ and Fe2+ around the OH groups in micas. J. Phys. C: Solid-State Phys. 16, 12711281.CrossRefGoogle Scholar
Sanz, J. & Stone, W.E.E. (1983b) NMR applied to minerals: IV. Local order in the octahedral sheet of micas: Fe-F avoidance. Clay Miner. 18, 177186.CrossRefGoogle Scholar
Thompson, J.B. (1981) Polytypism in complex crystals. Pp. 175196 in: Structure and Bonding in Crystals. II. (O'Keeffe, M. Navrotsky, A., editors). Academic Press, N.Y.Google Scholar