Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-24T17:16:26.906Z Has data issue: false hasContentIssue false

A note on kyanite in the Moine Series of Southern Ross-shire, and a review of related rocks in the Northern Highlands of Scotland

Published online by Cambridge University Press:  01 May 2009

T. N. Clifford
Affiliation:
Department of Geology, The University, Leeds, 2.

Abstract

New occurrences of kyanite-bearing schists in the Moine Series in southern Ross-shire demonstrate the order of appearance of the typomorphic minerals staurolite, kyanite, garnet, and sillimanite, and are of significance in elucidating the relationship of regional metamorphism to orogenesis. The scarcity of kyanite in the Northern Highlands is the result of both isochemical and allo-chemical effects, and its distribution is compared with that of its polymorphs andalusite and sillimanite.

Type
Articles
Copyright
Copyright © Cambridge University Press 1958

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

REFERENCES

Anderson, J. G. C., 1956. The Moinian and Dalradian Rocks between Glen Roy and the Monadhliath Mountains, Inverness-shire. Trans. Roy. Soc. Edin., lxiii, 1536.CrossRefGoogle Scholar
Barrow, G., 1893. On an Intrusion of Muscovite Biotile Gneiss in the S.E. Highlands of Scotland, and its accompanying Metamorphism. Quart. Journ. Geol. Soc., xlix, 330358.CrossRefGoogle Scholar
Barrow, G., 1912. On the Geology of Lower Deeside and the Southern Highland Border. Proc. Geol. Assoc., xxiii, 268284.CrossRefGoogle Scholar
Bosworth, T. O., 1910. Metamorphism around the Ross of Mull Granite. Quart. Journ. Geol. Soc., lxvi, 376401.CrossRefGoogle Scholar
Clark, S. P., and others, 1957. Experimental Determination of Kyanite Sillimanite Relations at High Temperatures and Pressures. Amer. Journ. Sci., cclv, 628640.CrossRefGoogle Scholar
Clifford, T. N., 1954. The stratigraphy and structure of parts of the Inverinate and Killilan Forests, southern Ross-shire; and the significance of the Kintail klippe in the tectonic interpretation of the Northern Highlands. Unpublished thesis for Ph.D. degree, Univ. of Leeds.Google Scholar
Clifford, T. N., 1957. The stratigraphy and structure of part of the Kintail district of southern Ross-shire: its relation to the Northern Highlands. Quart. Journ. Geol. Soc., cxiii, 5792.CrossRefGoogle Scholar
Francis, G. H., 1956. Facies Boundaries in Pelites at the Middle Grades of Regional Metamorphism. Geol. Mag., xciii, 353368.CrossRefGoogle Scholar
Halferdahl, L. B., 1957. Chloritoid. In Carnegie Inst. Washington Ann. Rept. of Geophysical Lab., No. 1277, 225–8.Google Scholar
Harker, A., 1939. Metamorphism. 2nd Edn., Methuen, London.Google Scholar
Harker, R. I., 1954. Further Data on the Petrology of the Pelitic Hornfelses of the Carn Chuinneag–Inchbae Region, Ross-shire, with special reference to the Status of Almandine. Geol. Mag., xci, 445462.CrossRefGoogle Scholar
Heddle, M. F., 1924. The Mineralogy of Scotland. Vol. II. St. Andrew's University Press.Google Scholar
Heitanen, Anna., 1956. Kyanite, andalusite, and sillimanite in the schist in Boehls Butte quadrangle, Idaho. Amer. Miner., xli, 127.Google Scholar
Horne, J., and others, 1914. The geology of the country round Beauly and Inverness. Mem. Geol. Surv. Scotland.Google Scholar
Kennedy, W. Q., 1955. The tectonics of the Morar Anticline and the problem of the North-West Caledonian Front. Quart. Journ. Geol. Soc., cx, 357390.Google Scholar
Korjinsky, D. S., 1937. Dependence of mineral stability on the depth. Soc. Russe Mineralogie Mem., 66, No. 2, 369396.Google Scholar
MacGregor, A. G., 1952. Metamorphism in the Moine Nappe of Northern Scotland. Trans. Edin. Geol. Soc., xv, 241257.CrossRefGoogle Scholar
MacGregor, A. G., 1953. In Summary of Progress of the Geological Survey of Great Britain for the year 1951, 44–6.Google Scholar
Miyashiro, A., 1949. The stability relation of kyanite, sillimanite, and andalusite and the physical condition of metamorphic processes Geol. Soc. Japan Journ., lv, 218223.Google Scholar
Peach, B. N. et al. , 1910. The geology of Glenelg, Lochalsh, and the south east part of Skye. Mem. Geol. Surv. Scotland.Google Scholar
Peach, B. N. et al. , 1912. The geology of Ben Wyvis, Carn Chuinneag, Inchbae, and the surrounding country. Mem. Geol. Surv. Scotland.Google Scholar
Peach, B. N. et al. , 1913. The geology of central Ross-shire. Mem. Geol. Surv. Scotland.Google Scholar
Phemister, J., 1948. British Regional Geology—Scotland: the Northern Highlands. 2nd Edn., Geol. Surv. and Mus.Google Scholar
Read, H. H., 1931. The geology of central Sutherland. Mem. Geol. Surv. Scotland.Google Scholar
Read, H. H. et al. , 1925. The geology of the country around Golspie, Sutherland shire. Mem. Geol. Surv. Scotland.Google Scholar
Read, H. H. et al. ,1926. The geology of Strath Oykell and Lower Loch Shin. Mem. Geol. Surv. Scotland.Google Scholar
Richey, J. E., 1931. In Summary of Progress of the Geological Survey of Great Britain for the year 1930, Pt. 1, 63–4.Google Scholar
Richey, J. E., and Kennedy, W. Q., 1939. The Moine and Sub-Moine Series of Morar, Inverness-shire. Bull. Geol. Surv. G.B., No. 2, 2645.Google Scholar
Thompson, J. B., 1955. The Thermodynamic Basis for the Mineral Facies Concept. Amer. Journ. Sci, ccliii, 65103.CrossRefGoogle Scholar
Tozer, C. F., 1955. The Mode of Occurrence of Sillimanite in the Glen District, Co. Donegal. Geol. Mag., xcii, 310320.CrossRefGoogle Scholar
Turner, F. J., and Verhoooen, J., 1951. Igneous and Metamorphic Petrology. Mcgraw-Hill, New York.Google Scholar
Winchell, A. N., 1951. Elements of Optical Mineralogy. Pt. II.Google Scholar