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Grandidierite from a pelitic xenolith in the Haddo House complex, NE Scotland

Published online by Cambridge University Press:  05 July 2018

R. K. Hero ,
B. F. Windley  and
D. Ackermand
R. K. Hero
Affiliation:
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A OE8, Canada
B. F. Windley
Affiliation:
Department of Geology, The University, Leicester LE1 7RH, United Kingdom
D. Ackermand
Affiliation:
Mineralogisches Institut der Universitäit, D-2300 Kid, Federal Republic of Germany
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Abstract

Grandidierite occurs in the outer margin of a biotite-rich pelitic xenolith in norite close to the contact of a tourmaline-bearing granite in the Haddo House norite-gabbro complex. The boron for the grandidierite was derived by metasomatism from the granite. The assemblage is (decreasing order): An55–51 plagioclase (65%), biotite (10%), spinel (10%), cordierite (5%), corundum (5%), ilmenite, grandidierite (< 1%), rutile, sphene, zircon. XMg range is grandidierite (0.80–0.78) > cordierite (0.78) > biotite (c. 0.59) > spinel (0.35–0.27). The grandidierite has little chemical variation: SiO2, 19.9–20.5%; Al2O3, 51.3–51.9%. A compilation of all grandidierite analyses in the literature shows that the only substitutions are Fe2+ ⇌ Mg and Al ⇌ Fe3+, the XMg range being 0.98 to 0.19.

Type
Research Article
Information
Mineralogical Magazine , Volume 48 , Issue 348 , September 1984 , pp. 401 - 406
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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References

Anderson, S. M. (1975) Ann. Rhod. Geol. Surv. 1, 49–59.Google Scholar
Black, P. M. (1970) Mineral. Mag. 37, 615-7.CrossRefGoogle Scholar
de Roever, E. W. F., and Kieft, C. (1976) Am. Mineral. 61, 332-3.Google Scholar
Grew, E. S. (1983) Mineral. Mag. 47, 401-3.CrossRefGoogle Scholar
Gribble, C. D. (1968) Contrib. Mineral. Petrol. 17, 315-30.CrossRefGoogle Scholar
Hamm, H. M., and Victen, K. (1971) Neues Jahrb. Mineral. Mh. 310-14.Google Scholar
Haslam, H. W. (1980) Mineral. Mag. 43, 822-3.CrossRefGoogle Scholar
Huijsmans, J. P. P., Barton, M., and van Bergen, M. J. (1982) Neues Jahrb. Mineral. Abh. 143, 249-61.Google Scholar
Krogh, E. (1975) Norsk Geol. Tidsskr. 55, 77–80.Google Scholar
Lacroix, A. (1922) Mineralogie de Madagascar, 1, A. Challamel, Paris, 624 pp.Google Scholar
Livingstone, A. and Macpherson, H. G. (1983) Mineral. Mag. 47, 99–106.CrossRefGoogle Scholar
McKie, D. (1965) Ibid. 34, 346–357.Google Scholar
Macpherson, H. G., and Livingstone, A. (1981) Scot. J. Geol. 18, 1–47.CrossRefGoogle Scholar
Olesch, M., and Seifert, F. (1976) Neues Jahrb. Mineral. Mh. 513-18.Google Scholar
Read, H. H. (1931) Geol. Mag. 68, 446-53.CrossRefGoogle Scholar
Read, H. H. (1935) Q. J. Geol. Soc. 91, 591–638.CrossRefGoogle Scholar
Seifert, F., and Olesch, M. (1977) Am. Mineral. 62, 547-53.Google Scholar
Semroud, B., Fabriès, J., and Conquere, F. (1976) Bull. Soc.fr. Mineral. Cristallogr. 99, 58–60.Google Scholar
Stephenson, D. A., and Moore, P. B. (1968) Acta Crystallogr. B24, 1518-22.CrossRefGoogle Scholar
van Bergen, M. J. (1980) Mineral. Mag. 43, 651-8.CrossRefGoogle Scholar
von Knorring, O., Sahama, Th. G., and Lehtinen, M. (1969) Bull. Geol. Soc. Finland. 41, 71-4.CrossRefGoogle Scholar
Vrána, S. (1979) Neues Jahrb. Mineral. Mh. 22–33.Google Scholar