Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-06T07:17:53.305Z Has data issue: false hasContentIssue false

The effect of fluorine and titanium on the vapour-absent melting of phlogopite and quartz

Published online by Cambridge University Press:  05 July 2018

J. A. K. Tareen
Affiliation:
Department of Studies in Geology, University of Mysore, Manasagangotri, Mysore-570 006, India
A. V. Keshava Prasad
Affiliation:
Department of Studies in Geology, University of Mysore, Manasagangotri, Mysore-570 006, India
B. Basavalingu
Affiliation:
Department of Studies in Geology, University of Mysore, Manasagangotri, Mysore-570 006, India
A. V. Ganesha
Affiliation:
Department of Studies in Geology, University of Mysore, Manasagangotri, Mysore-570 006, India

Abstract

Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Short Communications
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1995

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

Bohlen, S.R., Boettcher, A.L., Wall, V.J. and Clemens, J.D. (1983) Stability of phlogopite-quartz and sanidine-quartz: a model for melting in the lower crust. Contrib. Mineral. Petrol., 83, 270–7.CrossRefGoogle Scholar
Clemens, J.D. (1983) Experimental evidence against CO2 promoted deep crustal melting. Nature, 368, 336–8.Google Scholar
Clemens, J.D. and Wall, V.J. (1981) Crystallisation and origin of some paraluminous (S-type) granitic magmas. Canad. Mineral., 19, 111–32.Google Scholar
Essene, E.J. (1982) Geologic thermometry and barome-try. In. Mineralogical Society of America Reviews in Mineralogy, 10, 153–206.Google Scholar
Forbes, W.C. and Flower, M.F.J. (1974) Phase relations of titan-phlogopite, K2Mg4TiAl2Si6(OH)4: a refrac-tory phase in the upper mantle. Earth Planet. Sci. Lett., 22, 60–6.CrossRefGoogle Scholar
Goldmen, D.S. and Albee, A.L. (1977) Correlation of Mg/Fe partitioning between garnet and biotite with 18O/16O partitioning between quartz and magnetite. Amer. J. Sci., 277, 750–67.CrossRefGoogle Scholar
Grant, J.A. (1986) Quratz-phlogopite-liquid equilibria and origin of charnockites. Amer. Mineral., 71, 1071–5.Google Scholar
Harley, S.L. (1989) The origins of granulites: a metamorphic perspective. Geol. Mag., 126(3), 15-47.CrossRefGoogle Scholar
Montana, A. and Brearley, M. (1989) An appraisal of stability of phlogopite in the crust and the mantle. Amer. Mineral., 74, 1–4.Google Scholar
Peterson, J.W., Chacko, T. and Kuehner, S.M. (1991) The effects of fluorine on the vapour-absent melting of phlogopite + quartz: implications for deep crustal processes. Amer. Mineral., 76, 470–6.Google Scholar
Peterson, J.W. and Newton, R.C. (1989) Reversed experiments on biotite-quartz-feldspar melting in the system KMASH: implications for crustal anatexis. J. Geol, 97, 465–85.CrossRefGoogle Scholar
Shell, H.R. and Ivey, K.H. (1969) Fluorine micas. U.S. Bur. Mines Bull., 647, 291 pp.Google Scholar
Vielzeuf, D. and Clemens, J.D. (1992) The fluid-absent melting of phlogopite + quartz: experiments and models. Amer. Mineral., 77, 1206–22.Google Scholar