PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Powiadomienia systemowe
  • Sesja wygasła!
  • Sesja wygasła!
  • Sesja wygasła!
  • Sesja wygasła!
Tytuł artykułu

Geology and genesis of vein-type corundum deposits in the Hafafit-Nugrus area, South Eastern Desert, Egypt

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Unusual deposits formed by corundum are described from two separate pegmatitic veins in the Hafafit-Nugrus area of the South Eastern Desert of Egypt. Other related minerals are described too. The vein-type of corundum at Locality 1 (Vein 1) crosscuts through exposed rocks of an ophiolitic mélange, whereas at Locality 2 (Vein 2), it crosscuts through exposed serpentinised ultramafic rocks. The main minerals in Vein 1 are plagioclase, corundum, grossular, phlogopite, muscovite and clinochlore, while almandine, xenotime-(Y), allanite-(Ce), zircon, Cr-rich spinel, apatite, titanite, fergusonite-(Y), meta-ankoleite, U-rich thorite (uranothorite), carbonate and illite are the accessories. In Vein 2, the main minerals are plagioclase, corundum, phlogopite and chlorite, while clinochlore, euxenite-(Y), Nb-rich rutile, almandine, xenotime-(Y), allanite-(Ce), zircon, spinel, apatite, titanite, kasolite, dickite, illite, carbonate, antigorite and talc are accessories. The two types of corundum veins differ in their concentrations of Th, U, Zr, Nb, Ta, REE, Y and Li in wholerock compositions. Field observations, mineralogy and chemical analyses of samples from the two veins of corundum deposits, as well as concentrations of chromophore elements in corundum crystals, suggest metasomatic origins. The present study suggests that the two types of corundum veins formed at different ages from different residual magmas that underwent in-situ hybridisation with the host rocks.
Czasopismo
Rocznik
Strony
181--197
Opis fizyczny
Bibliogr. 52 poz.
Twórcy
  • Nuclear Materials Authority, Cairo, Egypt
autor
  • Nuclear Materials Authority, Cairo, Egypt
Bibliografia
  • Abduriyim, A. & Kitawaki, H., 2006. Determination of the origin of blue sapphire using Laser Ablation Inductively Coupled Plasma Mass Spectrometry. Journal of Gemology 30, 23–36.
  • Abu Elatta, S.A., 2007. Occurrence of rare metals deposits at Abu Kruq Area, South Eastern Desert, Egypt. Ain Ahams University, Egypt.
  • Abu Elatta, S.A. & Mansour, G.H., 2019. Petrogenesis, geodynamic and radioactivity of the granitic rocks of the Nugrus Weakness Zone, South Eastern Desert, Egypt. Acta Geologica Sinica, in press.
  • Abu Elatta, S.A. & Williams-Jones, A.E., 2018. Mineralogy and geochemistry studies on the Nusab El Balgum granitic batches, South Western Desert, Egypt. Arabian Journal of Geosciences 11, 556.
  • Abu Elatta, S.A., Khaleal, F.M. & Rashed, M.A., 2013. Characteristic of Madinat Nugrus peraluminous leucogranite carrier of radioactive minerals, Southeastern Desert, Egypt. Research Open Journal of Mineral and Mining Engineering 1, 15–34.
  • Anders, E. & Grevesse, N., 1989. Abundance of the elements: Meteoritic and solar. Geochimica et Cosmochimica Acta 53, 197–214.
  • Andrew Cowper, L., 1903. Plumasite, an oligoclase corundum rock, near Spanish Peak, California. University of California, Department of Geological Sciences Bulletin 3, 219–229.
  • Attendorn, H.G. & Bowen, R.N.C., 1997. Radioactive and stable isotope geology. Chapman & Hall, London, 87 pp.
  • Ballouard, C., Poujol, M., Boulvais, P., Branquet, P., Tartèse, R. & Vigneresse, J.L., 2016. Nb-Ta fractionation in peraluminous granites: a marker of the magmatic-hydrothermal transition. Geology 44, 231–234.
  • Boynton, W.V., 1984. Geochemistry of the rare earth elements: meteorite studies. In: Henderson, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, 63–114.
  • Bucher, K., Capitani, C. De. & Grapes, R., 2005. The development of a margarite–corundum blackwall by metasomatic alteration of a slice of mica schist in ultramafic rock, Kvesjöen, Norwegian Caledonides. The Canadian Mineralogist 43, 129–156.
  • Černý, P., Meintzer, R.E. & Anderson, A.I., 1985. Extreme fractionation in rare-element granitic pegmatites: Selected samples of data and mechanism. The Canadian Mineralogist 23, 381–421.
  • Cho, M., 1986. A kinetic study of clinochlore and its high temperature equivalent forsterite+cordierite-spinel at 2 kbar water pressure. American Mineralogist 71, 68–77.
  • El Ramly, M.F. & Greiling, R., 1988. Wadi Hafafit Area 1:100,000 Geological Map. Technische Fachhochschule, Berlin.
  • El Ramly, M.F., Greiling, R.O., Kroner, A.& Rashwan, A.A., 1984. On the tectonic evolution of Wadi Hafafit area and environs, Eastern Desert of Egypt. [In:] Proceedings of symposium on the Pan-African crustal evolution in the Arabian Shield, 113–126.
  • El Ramly, M.F., Greiling, R.O., Rashwan, A.A. & Rasmy, A.H., 1993. Explanatory note to accompany the geological and structural maps of Wadi Hafafit area, Eastern Desert of Egypt. Geological Survey of Egypt Paper 68.
  • El Sayed, R.M, Assran, H.M. & Abu Elatta S.A., 2014. Petrographic, radiometric and paleomagnetic studies for some alkaline rocks, south Nusab El Balgum mass complex, south Western Desert, Egypt. Geomaterials 4, 27–4.
  • Engel, A.E., Dixon, T.H. & Stern, R.J., 1980. Late Precambrian evolution of Afro-Arabian crust from ocean arc to craton. Bulletin of the Geological Society of America 91, 699–706.
  • Erlank, A.J., Marchant, J.W., Cardoso, M.P. & Ahrens, L.H., 1978. Zirconium. [In:] K.H. Wedepohl (Ed.): Handbook of Geochemistry. Springer, Part II, 40 pp.
  • Ewing, R.C., 1974. Mineralogy of metamict rare earth AB2O6-types Niobium-Tanalum-Titanium oxides. Stanford University, California, 45 pp.
  • Fritz, H., Dallmeyer., D.R., Wallbrecher, E., Loizenbauer, J., Hoinkes, G., Neumayr, P. & Khudeir, A.A., 2002, Neoproterozoic tectonothermal evolution of the Central Eastern Desert, Egypt: a slow velocity tectonic process of core complex exhumation. Journal of African Earth Sciences 34, 137–155.
  • Green, T.H., 1995. Significance of Nb/Ta as an indicator of geochemical processes in the crust–mantle system. Chemical Geology 120, 347–359.
  • Greiling, R.O., Abdeen, M.M., Dardir., A.A., El-Akhal, H., El-Ramly, M.F., Kamal El-Din G.M., Osman, A.F., Rashwan, A.A., Rice, A.H.N. & Sadek, M.F., 1994. A structural synthesis of the Proterozoic Arabian–Nubian Shield in Egypt. Geologische Rundschau 83, 484–501.
  • Greiling, R., Kroner, A. & El Ramly, M.F., 1984. Structural interference patterns and their origin in the Pan-African basement of the southeastern Desert of Egypt. [In:] A. Kröner & R. Greiling (Eds): Precambrian Tectonics Illustrated. Schweizerbart, Stuttgart, 40–412 pp.
  • Greiling, R., Kroner, A., El Ramly, M.F., El Akhal, H. & Stern, R.J., 1988. The tectonic evolution of the northwestern Red Sea margin as related to basement structure. Tectonophysics 153, 179–191.
  • Gurav, T., Chandrasekharam, D. & Singh, H.K., 2015. Trace Element and REE concentrations in the thermal waters, West Coast Geothermal Province, India. Proceedings World Geothermal Congress, Melbourne, 1–9.
  • Haapala, I., 1977. Petrography and geochemistry of the Eurajoki stock, a rapakivi-granite complex with greisen-type mineralization in southwestern Finland. Bulletin Geological Survey of Finland 286, 128 pp.
  • Hildreth, W., 1979. The Bishop Tuff: Evidence for the origin of compositional zonation in silicic magma chambers. Geological Society of America Special Paper 180, 43–74.
  • Hildreth, W., 1981. Gradients in silicic magma chamber: Implication for lithospheric magmatism. Journal of Geophysical Research 86, 10153–10192.
  • Irber, W., 1999. The lanthanide tetrad effect and its correlation with K/ Rb, Eu/ Eu*, Sr/ Eu, Y/ Ho and Zr/ Hf of evolving peraluminous granite suites. Geochimica et Cosmochimica Acta 63, 489–508.
  • Issawi, B., Francis, M., Youssef, A. & Osman, R., 2009: The Phanerozoic of Egypt: a geodynamic approach. Geological Survey of Egypt Special Publication 81, 589 pp.
  • Kosterin, A.V., Shevaleyevskii, I.D. & Kizyura, V.E., 1964. Behaviour of zirconium and hafnium in the pegmatites of the Kuramin Mountain Range. Geochemistry International 1, 989–993.
  • Lentz, D., 1996. U, Mo, REE mineralization in late tectonic granitic pegmatites, southwestern Grenville Province. Ore Geology Reviews 11, 197–227.
  • Linnen, R.L. & Keppler, H., 2002. Melt composition control of Zr/Hf fractionation in magmatic processes. Geochimica et Cosmochimica Acta 66, 3293–330.
  • Moghazi, A.M., Hassanein, M.A., Mohamed, F.H. & Ali, S., 2004. Late Neoproterozoic strongly peraluminous leucogranites, south Eastern Desert, Egypt. Petrogenesis and geodynamic significance. Mineralogy and Petrology 81, 19–41.
  • Peucat, J.J., Ruffault, P., Fritsch, E., Bouhnik-Le Coz, M., Simonet, C. & Lasnier, B., 2007. Ga/Mg ratios as a new geochemical tool to differentiate magmatic from metamorphic blue sapphires. Lithos 98, 261–274.
  • Pirajno, F., 1992. Hydrothermal mineral deposits. Principles and fundamental concepts for the exploration geologist. Springer-Verlag. Berlin, 1–155.
  • Pollard, D.D., 1973. Derivation and evaluation of a mechanical model for sheet intrusions. Tectonophysics 19, 233–269.
  • Rankin, A.H., Greenwood, J. & Hargreaves, D., 2003. Chemical fingerprinting of some East African gem rubies by Laser Ablation ICP-MS. Journal of Gemmology 28, 473–481.
  • Rudnick, R.L. & Fountain, D.M., 1995. Nature and composition of the continental crust: a lower crustal perspective. Reviews of Geophysics 33, 267–309.
  • Saminpanya, S., Manning, D. & Henderson, D., 2003. Trace elements in Thai gem corundums. Journal of Gemmology 28, 392–398.
  • Serencsists, C.M.C., Faul, H., Foland, K.A., El-Ramly, M.C. & Hussein, A.A., 1979. Alkaline ring complexes in Egypt: Their ages and relationship to tectonic development of the Red Sea. Annals of Geological Survey of Egypt 9, 102–116.
  • Serotta, A. & Carò, F., 2014. Evidence for the use of corundum abrasive in Egypt from the Great Aten Temple at Amarna. Horizon 14, 2–4.
  • Stoeser, D.B. & Camp, V.E., 1985. Pan-African microplate accretion of the Arabian Shield. Bulletin of Geological Society of America 96, 817–826.
  • Taylor, S.R. & McLennan, S.M., 1985. The continental crust: Its composition and evolution. Oxford, Blackwell, 312 pp.
  • Tomasic, N., Wang-Gajovic, A., Bermanec, V. & Rajic, M., 2004. Recrystallization of metamict Nb–Ta–Ti–REE complex oxides: A coupled X-ray-diffraction and Raman spectroscopy. The Canadian Mneralogist 42, 1847–1857.
  • Voudouris, P., Mavrogonatos, C. , Graham, I., Giuliani, G., Melfosm, V., Karampelas, V, Karantoni, V. Wang, K., Tarantola, A., Zaw, K., Meffre, S., Klemme, S., Berndt, J., Heidrich, S., Zaccarini, F., Fallick, A., Tsortanidis, M. & Lampridis, A., 2019. Gem corundum deposits of Greece: Geology, mineralogy and genesis. Minerals 9, 49–50.
  • Vlasov, K.A., 1966. Geochemistry and mineralogy of rare elements and genetic types of their deposits. I. Geochemistry of rare elements. Israel Program for Scientific Translations, Jerusalem, 688 pp.
  • Wang, L. & Liang, T., 2015. Geochemical fractions of rare earth elements in soil around a mine Tailing in Baotou, China. Scientific Reports, 5, https://doi.org/10.1038/12483.
  • Watson, E. & Harrison, T.M., 1983. Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types. Earth and Planetary Science Letters 64, 295–304.
  • Weyer, S., Musker, C., Rehkämper, M. & Mezger, K., 2002. Determination of ultra-low Nb, Ta, Zr and Hf concentrations and the chondritic Zr/ Hf and Nb/ Ta ratios by isotope dilution analyses with multiple collector CP-MS. Chemical Geology 187, 295–313.
  • Zharikov, V., Pertsev, N., Rusinov, V., Callegari, E. & Fettes, D., 2007. Metasomatism and metasomatic rocks. [In:] Fettes, D. & Desmons, J. (Eds): Metamorphic Rocks: A Classification and Glossary of Terms. Cambridge University Press, Cambridge, 58–68 pp.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-9045f791-1663-4879-a5a2-aab73e930b04
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.