Hostname: page-component-78c5997874-ndw9j Total loading time: 0 Render date: 2024-11-08T02:49:02.661Z Has data issue: false hasContentIssue false
  • English
  • Français

Geochemistry of ultramafic xenoliths and their host alkali basalts from Tallante, southern Spain

Published online by Cambridge University Press:  05 July 2018

C. Dupuy ,
J. Dostal  and
P. A. Boivin
C. Dupuy
Affiliation:
Centre Géologique et Géophysique, USTL, Place E. Bataillon, 34060 Montpellier Cedex, France Department of Geology, Saint Mary's University, Halifax, Nova Scotia, B3H 3C3, Canada Département de Géologie et Minéralogie, Université, 5 rue Kessler, 63038 Clermont-Ferrand Cedex, France
Get access Rights & Permissions [Opens in a new window]

Abstract

Ultramafic xenoliths enclosed in Plio-Quaternary alkali basalts from Tallante near Cartagne (southern Spain) are composed mainly of spinel lherzolites which are probably upper mantle residues. In many xenoliths, the spinel lherzolite is cut by pyroxenite or gabbroic anorthosite veinlets generally 0.2–3 cm thick. The clinopyroxenite veinlets were formed by high-pressure crystal-liquid segregation from alkali basalt magmas formed earlier than the host basalts, whereas mantle metasomatism played a role in the genesis of gabbroic anorthosites. Close to the contact with the veinlets, the spinel lherzolites are enriched in Ca, Fe, and some incompatible elements including light REE due to the migration of a fluid from the veinlets into the surrounding lherzolites. The host alkali basalts were derived from a heterogeneous, incompatible element-enriched upper-mantle source probably similar in composition and nature to the composite xenoliths, but were formed in a garnet stability field.

Keywords

geochemistryultramafic xenolithsbasaltsTallanteSpain
Type
Geochemistry
Information
Mineralogical Magazine , Volume 50 , Issue 356 , June 1986 , pp. 231 - 239
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1986

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

Alibert, C, Michard, A., and Albarede, F. (1983) The transition from alkali basalts to kimberlites: Isotope and trace element evidence from melilitites. Contrib. Mineral. Petrol, 82, 176-86.CrossRefGoogle Scholar
Boivin, P.A. (1982) Interaction entre magma basaltique et manteau superieur. Exemple du Deves (Massif Central francais) et du volcanisme quaternaire de la region de carthagene, Espagne. These Etat, Univ. de Clermont Ferrand, 344 pp.Google Scholar
Dostal, J., Dupuy, G, Carron, J.P., Le Guen de Kerneizon, M., and Maury, R.C. (1983) Partition coefficients of trace elements: application to volcanic rocks of St. Vincent, West Indies. Geochim. Cosmochim. Ada, 97, 525-33.CrossRefGoogle Scholar
Dupuy, C, Dostal, J., Liotard, J.M., and Leyreloup, A. (1980) Partitioning of transition elements between clinopyroxene and garnet. Earth Planet. Sci. Lett, 48, 303-10.CrossRefGoogle Scholar
Ehrenberg, S.N. (1982) Rare earth element geochemistry of garnet lherzolite and megacrystalline nodules from minette of the Colorado plateau province. Ibid. 57, 191-210.CrossRefGoogle Scholar
Fabries, J. (1979) Spinel-olivine geothermometry in peridotites from ultramafic complexes. Contrib. Mineral. Petrol. 69,329-36.Google Scholar
Frey, F.A. (1980) The origin of pyroxenites and garnet pyroxenites from Salt Lake Crater, Oahu, Hawaii: trace element evidence. Am. J. Sci, 280A, 427-49.Google Scholar
Frey, F.A. (1983) Rare earth element abundances in upper mantle rocks. In Rare earth element geochemistry (P. Henderson, ed.), 153-203. Elsevier, Amsterdam.Google Scholar
Frey, F.A. and Green, D.H. (1974) The mineralogy, geochemistry and origin of lherzolite inclusions in Victorian basanites. Geochim. Cosmochim. Ada, 38, 1023-59.CrossRefGoogle Scholar
Frey, F.A. and Prinz, M. (1978) Ultramafic inclusions from San Carlos, Arizona: Petrologic and geochemical data bearing on their petrogenesis. Earth Planet. Sci. Lett, 38, 129-76.CrossRefGoogle Scholar
Green, D.H., and Roy, S.D. (1978) Integrated models of basalt petrogenesis: a study of quartz tholeiites to olivine melilitites from South Eastern Australia utilizing geochemical and experimental petrological data. J. Petrol, 19, 463-513.Google Scholar
Gast, P.W. (1968) Trace element fractionation and the origin of tholeiite and alkaline magma types. Geochim. Cosmochim. Ada, 32, 1057-97.CrossRefGoogle Scholar
Glassley, W.E., and Piper, D.Z. (1978) Cobalt and scandium partitioning versus iron content for crystalline phases in ultramafic nodules. Earth Planet. Sci. Lett, 39, 173-8.CrossRefGoogle Scholar
Green, D.H., and Ringwood, A.E. (1967) The genesis of basaltic magmas. Contrib. Mineral. Petrol, 15, 102-90.CrossRefGoogle Scholar
Hanson, G.N. (1977) Geochemical evolution of the suboceanic mantle. J. Geol. Soc, London, 134, 235-53.CrossRefGoogle Scholar
Harris, P.G. (1957) Zone refining and the origin of potassic basalts. Geochim. Cosmochim. Ada, 12, 195-208.CrossRefGoogle Scholar
Hart, S.R., and Davis, K.E. (1978) Nickel partitioning between olivine and silicate melt. Earth Planet. Sci. Lett, 40, 203-19.CrossRefGoogle Scholar
Irving, A.J. (1974) Pyroxene-rich xenoliths in the Newer basalts of Victoria, Australia. Neues Jahrb. Mineral. Abh, 120, 147-67.Google Scholar
Irving, A.J. (1980) Petrology and geochemistry of composite ultramafic xenoliths in alkali basalts and implications for magmatic processes within the mantle. Am. J. Sci, 280A, 389-426.Google Scholar
Irving, A.J.and Price, R.C. (1981) Geochemistry and evolution of lherzolite-bearing phonolitic lavas from Nigeria, Australia, East Germany and New Zealand. Geochim. Cosmochim. Ada, 45, 1309-20.CrossRefGoogle Scholar
Jagoutz, E., Palme, H., Baddenhausen, H., Blum, K., Cendales, M., Dreibus, G., Spettel, B., Lorenz, V., and Wanke, H. (1979) The abundance of major, minor and trace elements in the earth's mantle as derived from primitive ultramafic nodules. Proc. 10th Lunar Sci. Conf., Geochim. Cosmochim. Ada, Suppl.11,2,2031-50.Google Scholar
Kay, R.W., and Gast, P.W. (1973) The rare earth content and the origin of alkali-rich basalt. J. Geol, 81, 653-82.CrossRefGoogle Scholar
Leeman, W.P., and Scheidegger, K.F. (1977) Olivine/ liquid distribution coefficients and a test for crystalliquid equilibrium. Earth Planet Sci. Lett, 35, 247-57.CrossRefGoogle Scholar
Lindstrom, D.J., and Weill, D.F. (1978) Partitioning of transition metals between diopside and coexisting silicate liquid. I. Nickel, cobalt and manganese. Geochim. Cosmochim. Ada, 42, 817-31.CrossRefGoogle Scholar
Lloyd, F.E., and Bailey, D.K. (1975) Light element metasomatism of the continental mantle: the evidence and the consequences. Phys. Chem. Earth, 9,389-416.Google Scholar
Maaloe, S., and Aoki, K. (1977) The major element composition of the upper mantle estimated from the composition of lherzolites. Contrib. Mineral. Petrol, 63, 161-73.CrossRefGoogle Scholar
Miller, C, and Richter, W. (1982) Solid and fluid phases in lherzolite and pyroxenite inclusions from the Hoggar, Central Sahara. Geochem. J, 16, 263-77.CrossRefGoogle Scholar
Mysen, B.O. (1979) Trace element partitioning between garnet peridotite mineral and water-rich vapor: Experimental data from 5 to 30 kb. Am. Mineral, 64, 274-87.Google Scholar
Obata, M. (1976) The solubility of A12O3 in orthopyroxenes in spinel and plagioclase peridotites and spinel pyroxenite. Ibid. 61, 804-16.Google Scholar
Onuma, N., Huguchi, H., Wakita, H., and Nagasawa, H. (1968) Trace element partition between two pyroxenes and the host lava. Earth Planet. Sci. Lett, 5, 47-51.CrossRefGoogle Scholar
Presnall, D.C. Dixon, S.A., Dixon, J.R., O'Donnel, T.H., Brenner, N.L., Schrock, R.L., and Dycus, D.W. (1978) Liquidus phase relations on the join diopsideforsterite- anorthite from 1 atm to 20 kb: their bearing on the generation and crystallization of basaltic magma. Contrib. Mineral. Petrol, 66, 203-20.CrossRefGoogle Scholar
Reid, J.B., Jr., and Woods, G.A. (1978) Oceanic mantle beneath the southern Rio Grande Rift. Earth Planet. Sci. Lett, 41, 303-16.CrossRefGoogle Scholar
Ringwood, A.E. (1975) Composition and petrology of the earth's mantle. McGraw-Hill, New York, 618 p.Google Scholar
Roeder, P.L., and Emslie, R.F. (1970) Olivine-liquid equilibrium. Contrib. Mineral. Petrol, 29, 275-89.CrossRefGoogle Scholar
Savoyant, L., Persin, F., and Dupuy, C. (1984) Determination des Terres Rares dans certaines Roches Basiques et Ultrabasiques. Geostand. Newsletter, 8, 159-61.CrossRefGoogle Scholar
Stosch, H.G. (1981) Sc, Cr, Co and Ni partitioning between minerals from spinel peridotite xenoliths. Contrib. Mineral. Petrol, 78, 166-74.CrossRefGoogle Scholar
Stosch, H.G. and Seek, H.A. (1980) Geochemistry and mineralogy of two spinel peridotite suites from Dreiser Weier, West Germany. Geochim. Cosmochim. Ada, 44, 457-70.CrossRefGoogle Scholar
Vielzeuf, D. (1983) The spinel and quartz associations in high grade xenoliths from Tallante (S. E. Spain) and their potential use in geothermometry and barometry. Contrib. Mineral. Petrol, 82, 301-11.CrossRefGoogle Scholar
Wass, S.Y. (1980) Geochemistry and origin of xenolithbearing and related alkali basaltic rocks from the Southern Highlands, New South Wales, Australia. Am. J. Sci, 280A, 639-66.Google Scholar
Wass, S.Y., and Rogers, N.W. (1980) Mantle meta- somatism—precursor to continental alkaline volcan- ism. Geochim. Cosmochim. Ada,, 44, 1811-.CrossRefGoogle Scholar
Wells, P.R.A. (1977) Pyroxene thermometry in simple xenoand complex systems. Contrib. Mineral. Petrol, 62, 129-39.CrossRefGoogle Scholar
Wendlandt, R.E. and Harrison, W.J. (1979) Rare earth partitioning between immiscible carbonate and silicate liquids and CO2 vapor: Results and implications for the formation of light rare earth enriched rocks. Ibid. 69, 409-19CrossRefGoogle Scholar
Wilshire, H.G., Pike, J.N. Myer, C.E., and Schwarzman, E. C. (1980) Amphibole-rich veins in lherzolite xeno liths, Dish Hill and Deadman Lake, California. Am. Jx Sri, 280A, 576-93.Google Scholar