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The composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria

Published online by Cambridge University Press:  05 July 2018

Y. Ahmid-Said
Affiliation:
Oum-Toub (Skikda). BP56. 21450. Algeria
B. E. Leake
Affiliation:
Department of Geology and Applied Geology, The University, Glasgow G12 800. U.K.

Abstract

The Kef Lakhal amphibolitcs and associated amphibolitc and olivine-rich enclaves are dcscribcd and their major and trace element chemistry indicates that both amphibolites were evolved medium to high alumina tholeiitic basalts with talc-alkaline affinities probably formed within plate settings. The olivine-rich enclaves are disrupted periodotites of the type lherzolite-harzburgite and probably represent mantle residua after melting.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1992

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Footnotes

Now Department of Geology and Applied Geology, The University, Glasgow G12 8QQ.

References

Ahmed-Said, Y. and Leake, B. E. (1992) The Cap de Garde pelites and gneisses; their geochemistry and origin (in press, Geological Survey of Algeria).Google Scholar
Banno, S. and Yoshino, G. (1965) Eclogite-bearing peridotite mass at Higasiakaisa-Yama in the Bess area, Central Sikoku, Japan. J. U.G.S. Upper Mantle Symposium, New Delhi, 150-60.Google Scholar
Coombs, D. S., Nakamura, Y. and Vuagnat, M. (1976) Pumpellyite-actinolite facies schists of the Taveyanne Formation near Loeche, Valais, Switzerland. J. Petrol., 17, 440–71.CrossRefGoogle Scholar
Dahl, P. S. (1980) The thermal-compositional depen-dence of Fe+2-Mg distributions between coexisting garnet and pyroxene: applications to geothermo-metry. Am. Mineral., 65, 854–66.Google Scholar
Deer, W. A., Howie, R. A. and Zussman, i. (1982) Rock-forming minerals. Vol 1A (Orthosilicates), Longman, London-New York.Google Scholar
Dickinson, W. R. (1974) Sedimentation within and beside ancient and modern magmatic arcs. In R. H. Dott and R. H. Shaver (eds): Modern and Ancient Geosyclinal Sedimentation: Doc. Eco. Pal. Min. Sp. Publ., 19, 230-9.CrossRefGoogle Scholar
Evans, B. W. and Leake, B. E. (1960) The composition and origin of the striped amphibolites of Connemara, Ireland. J. Petrol-, 1, 337–68.CrossRefGoogle Scholar
Fleet, M. E., MacRal, N. D., and Herzberg, C. T. (1977) Partition of nickel between olivine and sulfide: a test for immiscible sulfide liquids., Contrib. Mineral Petrol., 65, 191–8.CrossRefGoogle Scholar
Fourncll, H. (1849) Richesse minerale de l'Algerie, accompagnee d'e'claircissements historiques et geo-graphique sur cette partie de l'Afrique septentrio-nale. Imp. Nat. Paris., tl.Google Scholar
Ghent, E. D. (1976) Plagioclase-garnet-Al2SiO5-quartz: a potential geothermometer geobarometer. Am. Mineral., 61, 710–14.Google Scholar
Gleizes, G., Bouloton, J., Bossidre, G., and Collomb, P. (1988) Donndes lithologiques et pdtro-structurales nouvelles sur le massif cristallophyllien de l'Edough (Est-Algerien). C.R. Acad. Sci. Paris, 306(11), 1001-8.Google Scholar
Harvey, P. K., Taylor, D. M., and Hendry, R. D. (1973) An accurate fusion method for the analysis of rocks and chemically related minerals by X-ray fluorescence spectrometry. X-Ray Spectrometry, 2, 3346.CrossRefGoogle Scholar
Higgins, G. B. and Ribbe, P. H. (1977) The structure of malayaite, CaSnOSiO4, a tin analog of titanite. Am. Mineral., 62, 801–6.Google Scholar
Hilly, J. (1962) Etude gdologique du massif de l'Edough et du Cap de Fer (Est-Constantinois). Publ. Serv. Carte Gdol. Algerie (Nouvelles Sdrie), No. 19, pp. 408.Google Scholar
Hollister, L. S. (1966) Garnet zoning: an interpretation based on the Rayleigh fractionation model. Science, 154, 1647–51.CrossRefGoogle Scholar
Ilavsky, J. and Snopkovfi, P. (1987) DNcouverte d'Acri- tarches Paldozoiques dans les terrains mdtamor- phiques de l'Edough (Wilaya d'Annaba Algdrie). C.R. Acad. Sci. Paris, 305, 881–4.Google Scholar
Irvine, T. N. and Baragar, W. R. A. (1971) A guide to the chemical classification of the common volcanic rocks. Can. J. Earth Sci., 8, 523–48.CrossRefGoogle Scholar
Joleand, L. (1936) Service de la Carte Göologique de L'Algéria. Google Scholar
Kuno, H. (1966) Lateral variations of basalt magma type across continental margins and island arcs. Bull. Volcan., 29, 195222.CrossRefGoogle Scholar
Leake, B. E. (1964) Chemical distinction of ortho- and para-amphibolites. J. Petrol., 5, 238–54.CrossRefGoogle Scholar
Leake, B. E. (1972) Garnetiferous striped amphibolites from Connemara, Western Ireland. Mineral Mag., 38, 649–65.CrossRefGoogle Scholar
Leake, B. E. (1978) Nomenclature of amphiboles. Ibid., 42, 533–63.Google Scholar
Leake, B. E. Hendry, G. L., Kemp, A., Plant, A. G., Harvey, P. K., Wilson, J. R., Coats, J. S. Aucott, J. W., Lunel, T. and Howarth, R. J. (1969) The chemical analysis of rock powders by automatic X-ray fluores-cence. Chem. Geol., 5, 786.CrossRefGoogle Scholar
Macdonald, G. A. (1968) Composition and origin of Hawaiian lavas. Mem. Geol. Soc. Am., 116, 477522.Google Scholar
Manson, V. (1967) Geochemistry of basaltic rocks: major elements. In Hess, H. H. and Poldervaart, A. (eds): Basalts, 1, 215–6. J. Wiley, London.Google Scholar
Marignac, C. (1985) Les mindralisations filoniennes d'Ain Barbar (Algerie). Un Oxemple d'hydrothermalisme lid a I'activite gdothermique Alpine en Afrique du nord. Thése doctorat d'dtat (2 tomes), I. N. P. Loraine, Nancy, France.Google Scholar
Middlemost, E. A. K. (1985) Magma and magmatic rocks. Longman, London-New York, pp. 266.Google Scholar
Miyashiro, A. and Shido, F. (1975) Tholeiitic and calc-alkalic series in relation to the behaviors of titanium, vanadium, chromium and nickel. Am. J. Sci., 275, 265–77.CrossRefGoogle Scholar
Newton, R. C. and Haselton, H. T. (1981) Thermodynamics of minerals and melts. In Newton, R. C., Navrotsky, A. and Wood, B. J. (eds): Thermodynamics of minerals and melts. Springer-Verlag, New York, 131-47.CrossRefGoogle Scholar
O'Hara, M. J. and Mercy, E. L. P. (1963) Petrology and petrogenesis of some garnetiferous peridotites. Trans. Roy. Soc. Edinburgh, 65, 251314.CrossRefGoogle Scholar
Parran, A. (1883) Sur les t6rrains de gneiss des environs de BNne (Algérie). Bull. Soc. Gdol. Ft'., t.XI, 503-11.Google Scholar
Pearce, J. A. and Cann, J. R. (1973) Tectonic setting of basic volcanic rocks determined using trace element analyses. Earth Planet. Sci. Lett., 19, 290300.CrossRefGoogle Scholar
Perkins, D. and Newton, R. C. (1981) Charnockite geobarometers based on coexisting garnet- pyroxene-plagioclase-quartz. Nature, 292, 144–6.CrossRefGoogle Scholar
Renou, E. (1843) Aper∼u sur la constitution g4ologique de l'Algdrie. Ann. Mines, PaNs, 4e Sdrie (IV), 521-40.Google Scholar
Renou, E. (1848) Déscription géologique de l'Algérie, in 'exploration scientifique de l'Algdrie pendant les anndes ‘1840-1842'. Imp. Nat. Paris, I-IV and 1-164.Google Scholar
Sahama, T. G. (1946) On the chemistry of the mineral titanite. Bull. Comm. GNoL Finlande, 24, 88120.Google Scholar
Séligman-Lui, A. (1887-1890) Cartesgdologiques detail-lges de VAlgdrie au 1/50 000e, fcuilles 3-4 et 16-17: Béne-Bugeaud et notices explicatives. Arch. Serv. Carte. Géol. Algérie, Alger. (unpbl).Google Scholar
Séligman-Lui, A. and Ficheur, E. (1905) Ibid., feuille 16-17: Publ. Serv. Carte GNol. Algdrie, Alger.Google Scholar
Smith, J. V., and Stenstrom, R. C. (1965) Chemical analysis of olivines by the electron microprobe. Mineral Mag., 34, 436–59.Google Scholar
Thompson, A. B. (1976) Mineral reactions in pelitie rocks: II. calculation of some P-T-X (Fe-Mg) phase relations. Am. J. Sci., 276, 425–54.CrossRefGoogle Scholar
Van De Kamp, P. C. (1970) The Green Beds of the Scottish Dalradian series: geochemistry, origin, and metamorphism of mafic sediments. J. Geol., 78, 281303.CrossRefGoogle Scholar
Vila, J. M. (1970) Le Djebel Edough: Un massif cristallin externe due nord-est de la Berbérie. Bull. Soc. Gdol. Fr., (7), XII, 805-/2.CrossRefGoogle Scholar
Wilson, M. (1989) Igneous petrogenesis, a global tectonic approach. Unwin-Hyman, London, pp 466.CrossRefGoogle Scholar
Windley, B. F. (1977) The evolving continents (Second Edition): John Wiley and Sons.Google Scholar