Summary
The Alcsutdoboz-2 (AD-2) core contains 12 magmatic dykes which belong to the Late Cretaceous lamprophyric-carbonatitic association of NE Transdanubia, Hungary. Petrographically, 11 dykes can be considered alkaline lamprophyre (mainly monchiquite), and the remainder might be called carbonatite. The lamprophyre dykes are similar to both alkaline lamprophyres and ultramafic lamprophyres in major element composition, whereas the carbonatite dyke has some features that are similar to carbonatites but others that are dissimilar. Nevertheless, both of the two types of AD-2 dykes possess higher LILE content than the ultramafc lamprophyres and kimberlites, but strongly differ from average carbonatite. Based on the REE pattern, crystal fractionation (mainly of olivine) and separation of a carbonate phase from the parental lamprophyric magma are proposed for genesis of the carbonatite dyke. These characteristics and the compositional zoning of clinopyroxene and mica suggest a complex crystallization history for these dykes. The likeliest origin for the parental lamprophyric melt is through a very small degree of partial melting of metasomatized mantle.
Zusammenfassung
Der Kern der Bohrung Alcsutdoboz-2 (AD-2) enthält zwölf magmatische Gänge, die zu der jung-kretazischen Lamprophyr-Karbonatit-Assoziation des nordöstlichen Transdanubiens in Ungarn gehören. Petrographisch gesehen gehören elf Gänge zu den alkalischen Lamprophyren (hauptsächlich Monchiquit), und der Rest kann als Karbonatit bezeichnet werden. Die Lamprophyrgänge sind in ihrer Hauptelementzusammensetzung sowohl alkalischen Lamprophyren wie ultramafschen Lamprophyren ähnlich. Der Karbonatitgang hingegen zeigt Parameter, die denen von Karbonatiten teilweise, aber nicht durchwegs, ähnlich sind. Beide Typen der AD-2-Gänge zeigen höhere LILE-Gehalte als ultramafische Lamprophre und Kimberlite, unterscheiden sich aber deutlich vom durchschnittlichen Karbonatit. Auf der Basis der Seltenen ErdVerteilung, werden Kristallfraktionierung (hauptsächlich von Olivin) und Abtrennung einer Karbonatphase von lamprophyrischen Magma als Vorgänge gesehen, die für die Entstehung der Karbonatit-Gänge relevant sind. Diese Aspekte und die Zonierung der Zusammensetzungen von Klinopyroxen und Glimmer weisen auf eine komplexe Kristallisationsgeschichte dieser Gänge hin. Sehr wahrscheinlich ist die lamprophyrische Ausgangsschmelze durch eine geringfügige teilweise Aufschmelzung von metasomatisiertem Mantel entstanden.
Similar content being viewed by others
References
Akasaka M, Onuma K (1980) The join CaMgSi2O6-CaFeAlSiO6 CaTiAl2O6 and its bearing on the Ti-rich fassaitic pyroxenes. Contrib Mineral Petrol 71: 301–312
Aoki K (1971) Petrology of mafic inclusions from Itinomegata, Japan. Contrib Mineral Petrol 30: 314–330
—Kushiro I (1968) Some clinopyroxenes from ultramafic inclusions in Dreiser Weiher, Eifel. Contrib Mineral Petrol 18: 326–337
Arima M, Edgar AD (1981) Substitution mechanism and solubility of titanium in phlogopites from rocks of probable mantle origin. Contrib Mineral Petrol 77: 288–295
Bérczi J, Keömley G, Molnár Zs, Várkonyi T (1982) Detection and identification of emission source and the basis of the trace element composition of aerosols. Period Polytech 26: 123–137
Bergman SC (1987) Lamproites and other potassium-rich igneous rocks: a review of their occurrence, mineralogy and geochemistry. In:Fitton JG, Upton BGJ (eds) Alkaline rocks. Blackwell, Edinburgh, pp: 103–191
Bol LCGM, Bos A, Sauter PCC, Jansen JBH (1989) Barium-titanium-rich phlogopites in marbles from Rogaland, southwest Norway. Am Mineral 74: 439–447
Briqueu JC, Bougault H, Joron JL (1984) Quantification of Nb, Ta, Ti and V anomalies in magmas associated with subduction zones: petrogenetic implication. Earth Planet Sci Lett 68: 297–305
Clarke CB, Muecke GK, Pe-Piper G (1983) The lamprophyres of Ubekent Ejbund, West Greenland products of renewed partial melting or extreme differentiation. Contrib Mineral Petrol83: 117–127
Cooper AF (1979) Petrology of ocellar lamprophyres from western Otago, New Zealand. J Petrol 20: 139–163
Cullers RL, Graf JL (1984) Rare earth elements in igneous rocks of the continental crust: predominantly basic and ultrabasic rocks. In:Henderson P (ed) Developments in Geochemistry 2: Rare Earth Element Geochemistry. Elsevier, Amsterdam, pp. 237–274
Deer WA, Howei RH, Zussman J (1965) Rock Forming Minerals, Vol. 3. Longmans, London, p 270
Dobosi G, Horváth I (1988) High- and low-pressure cognate clinopyroxenes from the alkali lamprophyres of the Velence and Buda Mountains, Hungary. N Jb Min Abh 158: 241–256
Durazzo A, Taylor LA, Shervais JW (1984) Ultramafic lamprophyre in a carbonate platform environment, Mt. Queglia, Abruzzo, Italy. N Jb Min Abh 150: 199–217
Embey-Isztin A, Dobosi G, Noske-Fazekas G, Arva-Sós E (1989) Petrology of a new basalt occurrence in Hungary. Mineral Petrol 40: 183–196
Esperanca S, Holloway JR (1987) On the origin of some mica lamprophyres: experimental evidence from a mafic minette. Contrib Mineral Petrol 95: 207–216
Ferguson J, Currie KL (1971) Evidence of liquid immiscibility in alkaline ultrabasic dikes at Callander Bay Ontario. J Petrol 12: 561–585
Fesq HW, Kable EJD, Gurney JJ (1974) Aspects of the geochemistry of kimberlites from the Premier mine, and other selected South African occurrences with particular reference to the rare earth elements. Phys Chem Earth 9: 687–707
Forbes WC, Flower MFJ (1974) Phase relations of the titan-phlogopite, K2Mg4TiAl2Si2O (OH): a refractory phase in the upper mantle? Earth Planet Sci Lett 22: 60–66
Frey FA, Green DH, Roy SD (1978) Integrated models of basalt petrogenesis: A study of quartz tholeiites to olivine melilites from south eastern Australia utilizing geochemical and experimental petrological data. J Petrol 19: 463–513
Gaspar JC, Wyllie PJ (1982) Barium phlogopite from the Jacupiranga carbonatite, Brazil. Am Mineral 67:997–1001
— (1987) The phlogopites from the Jacupiranga carbonatite intrusions. Mineral Petrol 36: 121–134
Green DH (1970) The origin of basaltic and nephelinitic magmas. Trans Leicester Lit Phil Soc 64: 28–54
Guo J, Green TH (1990) Experimental study of barium partitioning between phlogopite and silicate liquid at upper-mantle pressure and temperature. Lithos 24: 83–95
Hamilton DL, Freenstone IC, Dawson JB, Donaldson CH (1979) Origin of carbonatites by liquid immiscibility. Nature 279: 52–54
Hansen K (1980) Lamprophyres and carbonatitic lamprophyres related to rifting in the Labrador Sea. Lithos 13: 145–153
Harrach O (1980) Petrology and geochemistry of magmatic rocks from Dinnyés-2, Diósd-1 and Vál-3 boreholes. (in Hungarian) M. Sc. Thesis, Department of Petrology and Geochemistry, Eötvös University, Budapest
Horváth.l, Darida-Tichy M, Odor L (1983) Magnesitiferous dolomitic carbonatite (beforsite) dyke rock from the Velence Mountains MAFI Evi jel 1981-röl: 369–389 (in Hungarian with English abstract)
—Odor L (1984) Alkaline ultramasic rocks and associated silicocarbonatites in the NE part of the Transdanubian Mts. (Hungary). Miner Slov 16: 115–119
Ito M (1986) Kimberlites and their ultramafic xenoliths from Western Kenya. Tscherm Miner Petrog Mitt 35: 193–216
Jaques AL, Sun SS, Chappell BW (1989) Geochemistry of the Argyle (AKI) lamproite pipe, Western Australia. In:Ross J (ed) Kimberlites and Related Rocks, Vol 1. Blackwell, Carlton, pp. 170–188
Kubovics I, Gál-Sólymos K, Szabó Cs (1985) Petrology and geochemistry of ultramafic xenoliths in mafic rocks of Hungary and Burgenland (Austria). Geol Carpathica 36: 433–450
—Szabó Cs, Gál-Sólymos K (1989a) A new occurrence of lamprophyre: Buda Mountains, Hungary. Acta Geol Hung 32: 149–168
—Szabó Cs, Gál-Sólymos K (1989b) Geochemistry of phlogopites in ultramafic xenoliths of lamprophyre dykes (Alcsutdoboz, Hungary). N Jb Min Abh 161: 171–191
Larsen JG (1981) Medium pressure crystallization of a monchiquitic magma—evidence from megacrysts of Drever's block, Ubekendt Ejland, West Greenland. Lithos 14: 241–262
Mansker WL, Ewing RC, Keil K (1979) Barium titanian biotites in nephelinites from Oahuu, Hawaii. Am Mineral 64:156–159
McDonough WF, Frey FA (1989) Rare earth elements in upper mantle rocks. In:Lipin BR, McKay GA (eds) Geochemistry and mineralogy of rare earth elements. Rev Mineral 21: 99–145
—,Frey FA McCulloch MT, Sun SS (1985) Isotopic and geochemical systematics in Tertiary—Recent basatts from southeastern Australia and implications for the evolution of the subcontinental lithosphere. Cosmochim Geochim Acta 49: 2051–2067
Meyer HOA, Mitchell RH (1988) Sapphire-bearing lamprophyre from Yogo Gulch, Montana—an ouachitite. Canad Mineral 26: 81–86
Mitchell RH (1981) Titaniferous phlogopites from the leucite-lamproites the West Kimberley area, Australia. Contrib Mineral Petrol 76: 243–251
— (1986) Kimberlites. Plenum Press, New York
—Bergman SC (1991) Petrology of lamproites. Planum Press, New York
—Platt RG (1984) The Freemans Cove volcanic suite: field relations, petrochemistry and tectonic setting of nephelinite-basanite volcanism associated with rifting the Canadian Artic archipelego. Can J Earth Sci 21: 428–436
Morimoto N, Fabries J, Ferguson AK, Ginzburg IV, Ross M, Seifert FA, Zussman J, Aoki K, Gottardi G (1988) Nomenclature of pyroxenes. Am Mineral 73: 1123–1133
Nagy-Balogh J, Hoffman L (1988) Study of Be-enriched volcanic tuffs by optical emission and atomic absoption sprectroscopy. 31th Hung Spear Meeting Abstract 329–332 (in Hungarian)
Olafsson M, Eggler DH (1983) Phase relations of amphibole, amphibole-carbonate, and phlogopite-carbonate peridotite; Petrologic constraints on the astenosphere. Earth Planet Sci Lett 64: 305–315
Papike JJ, Cameron KL, Baldvin K (1974) Amphiboles and pyroxenes: characterization of other than quadrilateral components and estimates of ferric iron from microprobe data. GSA Abstracts with programs 6: 1053–1054
Pearce JA (1983) Role of the sub-continental lithosphere in magma genesis at active continental margins: In:Hawkesworth CJ, Norry MJ (eds) Continental Basalts and Mantle Xenoliths, Shiva, Cheshire, pp. 230–249
Philpotts AR (1976) Silicate liquid immiscibility: its probable extent and petrogenetic significance. Am J Sci 276: 1147–1177
Praegel ND (1981) Origin of ultramafic inclusions and megacrysts in a monchiquite dyke at Streap, Inverness-shire, Scotland. Lithos 14: 305–322
Robert JL (1976) Titanium solubility in synthetic phlogopite solid solutions. Chem Geol 17: 213–227
Rock NMS (1977) The nature and origin of lamprophyres: some definitions, distinctions, and deviations. Earth Sci Rev 13: 123–169
— (1987) The nature and origin of lamprophyres: an overview. In:Fitton JG, Upton BGJ (eds) Alkaline Igneous Rocks. Blackwell, Edinburgh, pp 191–226
Rowell WF, Edgar AD (1983) Cenozoic potassium rich mafc volcanism in the western U.S.A.: its relationship to deep subduction. J Geol 91: 338–341
Smith J V, Delaney JS, Hervig RL, Dawson JB (1981) Storage of F and Cl in the upper mantle: geochemical implications. Lithos 14: 133–147
Solie DN, Su SC (1987) An occurrence of Ba-rich micas from the Alaska Range. Am Mineral 72:995–999
Streckeisen A (1979) Classification and nomenclature of volcanic rocks, lamprophyres, carbonatites and melilitic rocks. Geology 7: 331–335
Szabó Cs (1984) Mineralogy, petrology and geochemistry of ultramafc nodules in lamprophyre dykes of Alcsutdoboz-2 borehole (Bakonyicum, Hungary): their origin and genetic implications. Doctoral Thesis (in Hungarian) Department of Petrology and Geochemistry, Eötvös University, Budapest
— (1985) Xenoliths from Cretaceous lamprophyres of Alcsutdoboz-2 borehole, Transdanubian Central Mountains, Hungary. Acta Mineral Petrogr Szeged 27: 39–50
Thompson RN (1974) Some high-pressure pyroxenes. Mineral Mag 39: 768–787
— (1977) Primary basalts and magma genesis III Alban Hills, Roman comagmatic province, central Italy. Contrib Mineral Petrol 60: 91–108
Tracy RJ (1991) Ba-rich micas from the Franklin Marble, Lime Crest and Sterling Hill, New Jersey. Am Mineral 76:1683–1693
Tronnes RG, Edgar AD, Arima M (1985) A high pressure—high temperature study of TiO2 solubility in Mg-rich phlogopite: implications to phlogopite chemistry. Geochim Cosmochim Acta 49: 2323–2329
Velde D (1979) Trioctahedral mica in melilite-bearing eruptive rocks. Carnegie Inst Washington Yearb 78: 468–475
Wass SY (1979) Multiple origins of clinopyroxenes in alkali basaltic rocks. Lithos 12: 115–132
Wendlandt RF (1977) Barium phlogopite from Haystack Butte, Highwood Mountains, Montana. Carnegie Inst Washington Yearb 76: 534–539
—Harrison WJ (1979) Rare earth partitioning between immiscible carbonate and silicate liquids and C02 vapor: results and implications for the formation of light rare earthenriched rocks. Contrib Mineral Petrol 69: 409–419
Wilkinson JFG (1975) Ultramafic inclusions and high pressure megacrysts from a nephelinite sill, Nandewar Mountains, North-Eastern New South Wales, and their bearing on the origin of certain inclusions in alkaline volcanic rocks. Contrib Miner Petrol 51: 235–262
Wilson M (1989) Igneous petrogenesis. Unwin Hyman, London
Woolley AR, Kempe DRC (1989) Carbonatites: Nomenclature, average chemical compositions, and element distributions. In:Bell K (ed) Carbonatites: Genesis and Evolution. Unwin Hyman, London, pp. 1–14
Zentai P (1967) Spectrochemical methods for geochemical purposes. Acta Chim Hung 53: 323–333
Yagi K, Onuma K (1967) The join CaMgSi2O6-CaTiAl2O6 and its bearing on the titanaugites. J Fac Sci Hokkaido Univ Ser 4 13: 463–483
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Szabó, C., Kubovics, I. & Molnár, Z. Alkaline lamprophyre and related dyke rocks in NE Transdanubia, Hungary: The Alcsutdoboz-2 (AD-2) borehole. Mineralogy and Petrology 47, 127–148 (1993). https://doi.org/10.1007/BF01161563
Issue Date:
DOI: https://doi.org/10.1007/BF01161563