کیانیت در هاله‌های دگرگونی

[1] Akaad, M. K., The Ardara granitic diapir of Co. Donegal, Ireland. Geological Society of London Quaternary Journal. 112, (1956a) 263-88.

[2] Akaad, M. K., The northern aureole of the Ardara pluton of County Donegal. Geological Magazine. 93, (1956b) 377-92.

[3] Atkin, B. P., A mineralogical and chemical study of the paragenesis of opaque minerals in the Donegal granites and their aureole rocks, Eire. Ph.D. thesis, University of Liverpool. (1977)

[4] Atherton, M.P., Naggar, M,H., and Pitcher, W.S., Kyanite in some thermal aureoles. American Journal of Sciences, 275, (1975) 432-443.

[5] Barnicoat, A.C., and Prior, D, J., (ms.). Contact metamorphism around the Ross of Mull granite, scotland.

[6] Berger, A.R., The Main Donegal granite and its regional setting: a study of its fabric and structural relationships. Ph.D. thesis, University of Liverpool.

(1967)

[7] Delor. C.P., Burg, J.P., and Leyreloup, A.F., Staurolite producing reactions and geothermobarometry of a high pressure thermal aureole in the France Massif Central. Journal of Metamorphic Geology, 2, (1984) 55-72.

[8] Edmunds, W. M., A chemical and mineralogical study of pelitic hornfelses associated with certain granites of County Donegal.

Ph.D. thesis, University of Liverpool. (1969)

[9] Flinn, D., Key, R.M., and Khoo, T.T., The chloritoid schists of Shetland and their thermal metamorphism. Scottish Journal of Geolgy, 32, (1996) 67-82.

[10] Guidotti, C.V. Triple Point Assemblage. (2000, July 17)

http://www. mailbase. ac. uk /lists/geo-metamorphism/2000-07/0018.html, WWW:Mailbase.ac.uk. [11] Hodges, K.V., and Spear, F.S., Geothermometry, geobarometry and the Al2SiO5 triple point at Mt. Moosilauke, new Hampshire. American Mineralogist, 67, (1982) 1118-1134.

[12] Holdaway, M.J., Stability of andalusite and the aluminium silicate phase diagram. American Journal of Sciences, 271, (1971) 97-131.

[13] Holder, M. T., An emplacement mechanism for post-tectonic granites and its implications for their geochemical features. In: Atherton, M.P. and Tarney, J. (ads.), origin of Granite Batholiths. Geochemical Evidence, (1979) 116-128, Shiva, Orpington.

[14] Hollister, L.S. Contact metamorphism in the Kwoiek area of British Columbia: an end member of the metamorphic process. Geological Society of America Bulletin, 80, (1969a) 2465-2494.

[15] Hollister, L.S., Metastable paragenetic sequence of andalusite, kyanite and sillimanite, Kwoiek area, British Columbia. American Journal of Sciences, 267,

(1969b) 352-370.

[16] Homam, S. M., A chemical and textural study of aluminium silicate-bearing rocks from the contact aureole of the Ardara pluton, Co. Donegal, Ireland. Ph.D Thesis, University of Liverpool. (2000)

[17] Kerrick, D. M., Fibrolite in contact aureoles of Donegal, Ireland. American Mineralogist. 72, (1987) 240-254.

[18] Kerrick, D.M., The Al2SiO5 polymorphs. Reviews in Mineralogy, 22,

(1990) 406p.

[19] Loomis, T.P., Contact metamorphism of pelitic rock by the Ronda ultramafic intrusion, southern Spain. Geological Society of America Bulletin, 83, (1972a) 2449-2474.

[20] Loomis, T.P., Coexisting aluminum silicate phases in contact metamorphic aureoles. American Journal of Sciences, 272, (1972b) 933-945.

[21] Mangan, L.S., Equilibrium and disequilibrium aspects of contact metamorphism: The Ross of Mull Granite aureole, Scotland. Ph.D Thesis,University of Liverpool. (1996)

[22] Naggar, M. H., Aureole rocks from Co. Donegal Eire. Ph.D Thesis, University of Liverpool. (1968)

[23] Naggar, M. H. and Atherton, M. P., The composition and metamorphic history of some aluminum silicate-bearing rocks from the aureoles of the Donegal granites. Journal of Petrology. 11, (1970) 549-589.

[24] Pattison, D.R.M., and Tracy, R.J., Phase equilibria and thermobarometry of metapelites. In Reviews in Mineralogy, (1991) 26: Contact metamorphism (ed. D.M. Kerrick), pp. 105-206. Mineralogical Society of America.

[25] Pitcher, W. S. and Berger, A. R., The geology of Donegal: A study of Granite Emplacement and Unroofing. John Wiley, New York, (1972) 435p.

[26] Pitcher, W. S. and Read, H. H., The Main Donegal granite. Geological Society of London Quaternary Journal, (1959) 114, 259-305.

[27] Pitcher, W.S. and Read, H.H., Contact metamorphism in relation to manner of emplacement of the granites of Donegal, Ireland. Journal of Geology. 71,

(1963) 261-96.

[28] Pitcher, W.S. and Sinha, R.C., The petrochemistry of the Ardara aureole. Geological Society of London Quaternary Journal, 113, (1958) 393-408.

[29] Pitcher, W.S. and Read, H.H., The aureole of the Main Donegal granite. Geological Society of London Quaternary Journal, 116, (1960) 1-36.

[30] Spear, F.S., Triple Point Assemblage. (2000, July 16) http://www. Mailbase . ac.uk/ lists/geo -metamorphism/2000-07/0014.html, WWW: Mailbase.ac.uk.

[31] Vernon, R. H. and Paterson, S. R., The Ardara pluton, Ireland: deflating and expanded intrusion. Lithos, 31, (1993) 17-32.

[32] Yardley, B.W.D. and Long, C. B., Contact metamorphism and fluid movement around the Easky adamellite, Ox Mountains, Ireland. Mineralogical Magazine. 44, (1981) 125-131.

[33] Yardley, B.W.D. Triple Point Assemblage. (2000, July 17) http ://www .mailbase . ac. uk/lists/geo-metamorphism/2000-07/0022.html, WWW:Mailbase.ac.uk.

[34] Pattison, D.R.M., Al2SiO5 localities. (2000, July 21) http://www.mailbase.ac.uk/ lists/geo-metamorphism/2000-07/0043.html, WWW:Mailbase.ac.uk.