Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-26T17:33:25.389Z Has data issue: false hasContentIssue false

REE partitioning between apatite and melt in a peralkaline volcanic suite, Kenya Rift Valley

Published online by Cambridge University Press:  05 July 2018

R. MacDonald*
Affiliation:
IGMiP Faculty of Geology, University of Warsaw, Al. , Żwirki i Wigury 93, 02-089 Warsaw , Poland Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK
B. Baginíski
Affiliation:
IGMiP Faculty of Geology, University of Warsaw, Al. , Żwirki i Wigury 93, 02-089 Warsaw , Poland
H. E. Belkin
Affiliation:
U.S. Geological Survey, 956 National Center, Reston, VA 20192, USA
P. Dzieržanowski
Affiliation:
IGMiP Faculty of Geology, University of Warsaw, Al. , Żwirki i Wigury 93, 02-089 Warsaw , Poland
L. Jeżak
Affiliation:
IGMiP Faculty of Geology, University of Warsaw, Al. , Żwirki i Wigury 93, 02-089 Warsaw , Poland
*

Abstract

Electron microprobe analyses are presented for fluorapatite phenocrysts from a benmoreite-peralkaline rhyolite volcanic suite from the Kenya Rift Valley. The rocks have previously been well characterized petrographically and their crystallization conditions are reasonably well known. The REE contents in the M site increase towards the rhyolites, with a maximum britholite component of ~35 mol.%. Chondrite-normalized REE patterns are rather flat between La and Sm and then decrease towards Yb. Sodium and Fe occupy up to 1% and 4%, respectively, of the M site. The major coupled substitution is REE3+ + Si4+ ↔ Ca2+ + P5+. The substitution REE3+ + Na+ ↔ 2Ca2+has been of minor importance. The relatively large Fe contents were perhaps facilitated by the low fO2conditions of crystallization. Zoning is ubiquitous and resulted from both fractional crystallization and magma mixing. Apatites in some rhyolites are relatively Y-depleted, perhaps reflecting crystallization from melts which had precipitated zircon. Mineral/glass (melt) ratios for two rhyolites are unusually high, with maxima at Sm (762, 1123).

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

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

Andersen, D.J., Lindsley, D.H. and Davidson, P.M. (1993) QUILF: a Pascal program to assess equilibria among Fe-Mg-Ti oxides, pyroxenes, olivine and quartz. Computers & Geosciences, 19, 13331350.CrossRefGoogle Scholar
Armstrong, J.T. (1995) CITZAF: A package of correction programs for the quantitative electron microbeam X-ray analysis of thick polished materials, thin films, and particles. Microbeam Analysis, 4, 177200.Google Scholar
Boyce, J.W. and Hervig, R.L. (2009) Apatite as a monitor of late-stage magmatic processes at Volcan Irazu, Costa Rica. Contributions to Mineralogy and Petrology, 157, 135145.CrossRefGoogle Scholar
Biihn, B., Wall, F. and Le Bas, M.J. (2001) Rare-earth element systematics of carbonatitic fluorapatites, and their significance for carbonate magma evolution. Contributions to Mineralogy and Petrology, 141, 572591.CrossRefGoogle Scholar
Cherniak, DJ. (2000) Rare earth element diffusion in apatite. Geochimica et Cosmochimica Ada, 64, 38713885.CrossRefGoogle Scholar
Clarke, M.C., Woodhall, D.G., Allen, D. and Darling, G. (1990) Geological, volcanological and hydrogeological controls on the occurrence of geothermal activity in the area surrounding Lake Naivasha, Kenya. Ministry of Energy Report, Nairobi, Kenya, 138 pp.Google Scholar
Comodi, P., Liu, Y., Stoppa, F. and Woolley, A.R. (1999) A multi-method analysis of Si-, S- and REE-rich apatite from a new find of kalsilite-bearing leucitite (Abruzzi, Italy). Mineralogical Magazine, 63, 661672.CrossRefGoogle Scholar
Exley, R.A. (1980) Microprobe studies of REE-rich accessory minerals: implications for Skye granite petrogenesis and REE mobility in hydrothermal systems. Earth and Planetary Science Letters, 48, 97110.CrossRefGoogle Scholar
Fransolet, A.-M. and Schreyer, W. (1981) Unusual, iron-bearing apatite from a garnetiferous pegmatoid, Northampton Block, Western Australia. Neues Jahrbuch fur Mineralogie Monatshefte, 317327.Google Scholar
Heumann, A. and Davies, G.R. (2002) U-Th disequilibrium and Rb-Sr age constraints on the magmatic evolution of peralkaline rhyolites from Kenya. Journal of Petrology, 43, 557577.CrossRefGoogle Scholar
Hughes, J.M., Cameron, M. and Mariano, A.N. (1991) Rare-earth-element ordering and structural variations in natural rare-earth-bearing apatites. American Mineralogist, 76, 11651173.Google Scholar
Macdonald, R. and Bailey, D.K (1973) The chemistry of the peralkaline oversaturated obsidians. U.S. Geological Survey Professional Paper, 440-N-l, N1N37.Google Scholar
Macdonald, R., Davies, G.R., Bliss, CM., Leat, P.T., Bailey, D.K. and Smith, R.L. (1987) Geochemistry of high-silica rhyolites, Naivasha, Kenya rift valley. Journal of Petrology, 28, 9791008.CrossRefGoogle Scholar
Macdonald, R., Belkin, H.E., Fitton, J.G., Rogers, N.W., Nejbert, K., Tindle, A.G. and Marshall, A.S. (2008) The roles of fractional crystallization, magma mixing, crystal mush remobilization and volatile-melt interactions in the genesis of a young basalt—peralkaline rhyolite suite, the Greater Olkaria Volcanic Complex, Kenya Rift Valley. Journal of Petrology, 49, 15151547.CrossRefGoogle Scholar
Mahood, G.A. and Hildreth, W. (1983) Large partition coefficients for trace elements in high-silica rhyo lites. Geochimica et Cosmochimica Ada, 47, 11 —30.CrossRefGoogle Scholar
Mahood, G.A. and Stimac, J.A. (1990) Trace-element partitioning in pantellerites and trachytes. Geochimica et Cosmochimica Ada, 54, 22572276.CrossRefGoogle Scholar
Mandarino, J.A. (1999) Fleischer's Glossary of Mineral Species. The Mineralogical Record Inc. Tucson, Arizona, USA, 225 pp.Google Scholar
Marshall, A.S., Macdonald, R., Rogers, N.W., Fitton, J.G., Tindle, A.G., Nejbert, K. and Hinton, R.W. (2009) Extreme fractionation of peralkaline silicic magmas :the Greater Olkaria Volcanic Complex, Kenya Rift Valley. Journal of Petrology, 50, 323359.CrossRefGoogle Scholar
Oberti, R., Ottolini, L., Delia Ventura, G. and Parodi, G.C. (2001) On the symmetry and crystal chemistry of britholite: New structural and microanalytical data. American Mineralogist, 86, 10661075.CrossRefGoogle Scholar
Pan, Y. and Fleet, M.E. (2002) Compositions of the apatite-group minerals: substitution mechanisms and controlling factors. Pp. 13–49 in: Phosphates: Geochemical, Geobiological, and Materials Importance (Kohn, M.J., Rakovan, J. and Hughes, J.M., editors). Reviews in Mineralogy and Geochemistry 48, Mineralogical Society of America, Chantilly, Virginia, USA.Google Scholar
Piccoli, P.M. and Candela, P.A. (2002) Apatite in igneous systems. Pp. 255–292 in: Phosphates: Geochemical, Geobiological, and Materials Importance (Kohn, MJ., Rakovan, J. and Hughes, J.M., editors). Reviews in Mineralogy and Geochemistry, 48, Mineralogical Society of America, Chantilly, Virginia, USA.Google Scholar
Roeder, P.L., McArthur, D., Ma, X.P. and Palmer, G.R. (1987) Cathodoluminescence and mieroprobe study of rare-earth elements in apatite. American Mineralogist, 72, 801811.Google Scholar
Ronsbo, J.G. (1989) Coupled substitutions involving REEs and Na and Si in apatites from alkaline rocks from the Ilimaussaq intrusion, South Greenland, and the petrological implications. American Mineralogist, 74, 896901.Google Scholar
Ronsbo, J.G. (2008) Apatite in the Ilimaussaq alkaline complex: Occurrence, zonation and compositional variation. Lithos, 106, 7182.CrossRefGoogle Scholar
Scaillet, B. and Macdonald, R. (2001) Phase relations of peralkaline silicic magmas and petrogenetic implications. Journal of Petrology, 42, 825845.CrossRefGoogle Scholar
Scaillet, B. and Macdonald, R. (2003) Experimental constraints on the relationships between peralkaline rhyolites of the Kenya Rift Valley. Journal of Petrology, 44, 18671894.CrossRefGoogle Scholar
Sha, L.-K. and Chappell, B.W. (1999) Apatite chemical composition, determined by electron mieroprobe and laser-ablation inductively coupled plasma mass spectrometry, as a probe into granite petrogenesis. Geochimica et Cosmochimica Ada, 63, 38613881.CrossRefGoogle Scholar
Sun, S.-S. and McDonough, W.F. (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Pp. 313–345 in: Magmatism in the Ocean Basins (Saunders, A.D. and Norry, M.J., editors). Geological Society, London, Special Publication, 42.Google Scholar
Tepper, J.H. and Kuehner, S.M. (1999) Complex zoning in apatite from the Idaho batholith: A record of magma mixing and intracrystalline trace element diffusion. American Mineralogist, 84, 581595.CrossRefGoogle Scholar
Wilding, M.C., Macdonald, R., Davies, J.E. and Fallick, A.E. (1993) Volatile characteristics of peralkaline rhyolites from Kenya: an ion mieroprobe, infrared spectroscopic and hydrogen isotope study. Contributions to Mineralogy and Petrology, 144, 264275.CrossRefGoogle Scholar
Supplementary material: File

Macdonald et al. supplementary material

Supplementary data table 1

Download Macdonald et al. supplementary material(File)
File 134.7 KB
Supplementary material: File

Macdonald et al. supplementary material

Supplementary data table 2

Download Macdonald et al. supplementary material(File)
File 180 Bytes
Supplementary material: File

Macdonald et al. supplementary material

Supplementary data table 3

Download Macdonald et al. supplementary material(File)
File 49.7 KB