The Tellnes ilmenite deposit (Rogaland, South Norway): magnetic and petrofabric evidence for emplacement of a Ti-enriched noritic crystal mush in a fracture zone
titanium deposit; petrofabric; anisotropy of magnetic susceptibility (AMS); Rogaland, Norway
Abstract :
[en] The Tellnes ilmenite deposit, a world class titanium deposit, occurs in the Ana-Sira anorthosite (Rogaland anorthosite province, South Norway). It is mainly made up of an ilmenite-rich norite that has been previously interpreted as injected in a crystal mush state, in a weakness zone of the enclosing anorthosite. This emplacement mechanism has produced a faint orientation in the ore due to the flow of the mush. The internal flow structure of the orebody is studied here using the low-field anisotropy of magnetic susceptibility (AMS) method. Partial anhysteretic remanent magnetization (pAARM) indicates that coarse magnetite is the main mineral responsible for the magnetic fabric. Parallelism of the magnetic fabric with the shape-preferred orientation of the ore-forming minerals is checked using image analysis (IA) from oriented sections (intercept method). Interpretation of the AMS data verified by pAARM and IA, provides information on the magmatic foliation and lineation. Emplacement flow of the ilmenite norite crystal mush occurred in the direction of the orebody, parallel to its walls, and with an average SE 18degrees plunge. The feeder zone was likely situated below a network of veins on the SE end of the orebody. The sickle-shaped outcrop of the deposit suggests a transcurrent, dextral opening of a WNW-ESE-striking weakness zone across the anorthosite pluton. (C) 2002 Elsevier Science Ltd. All rights reserved.
Disciplines :
Physical, chemical, mathematical & earth Sciences: Multidisciplinary, general & others
Author, co-author :
Diot, Hervé; Université de La Rochelle
Bolle, Olivier ; Université de Liège - ULiège > Département de géologie
Lambert, Jean-Marc
Launeau, Patrick; Université de Nantes
Duchesne, Jean-Clair ; Université de Liège - ULiège > Dpt géologie > Pétrologie et géochimie endogènes
Language :
English
Title :
The Tellnes ilmenite deposit (Rogaland, South Norway): magnetic and petrofabric evidence for emplacement of a Ti-enriched noritic crystal mush in a fracture zone
Publication date :
2003
Journal title :
Journal of Structural Geology
ISSN :
0191-8141
Publisher :
Pergamon-Elsevier Science Ltd, Oxford, United Kingdom
Arbaret, L., Launeau, P., Diot, H., 2002. Significance of magnetic and three-dimensional Shape Preferred Orientation of magnetite in simple shear flow. Tectonophysics, in press.
Åreback, H., Stigh, S., 2000. The nature and origin of an anorthositic associated ilmenite-rich leuconorite, Hakefjorden Complex, south-west Sweden. Lithos 51, 247-267.
Barnichon, J.D., Havenith, H., Hoffer, B., Charlier, R., Jongmans, D., Duchesne, J.C., 1999. The deformation of the Egersund-Ogna anorthosite massif, south Norway: finite-element modeling of diapirism. Tectonophysics 303, 109-130.
Bingen, B., Demaiffe, D., van Breemen, O., 1998. The 616-My-old Egersund basaltic dike swarm, SW Norway, and late Proterozoic opening of the Iapetus Ocean. The Journal of Geology 106, 565-574.
Bolle, O., Diot, H., Duchesne, J.C., 2000. Magnetic fabric and deformation in charnockitic igneous rocks of the Bjerkreim-Sokndal layered intrusion (Rogaland, Southwest Norway). Journal of Structural Geology 22, 647-667.
Borradaile, G.J., Henry, B., 1997. Tectonic applications of magnetic susceptibility and its anisotropy. Earth-Science Reviews 42, 49-93.
Bouchez, J.L., 1997. Granite is never isotropic: an introduction to AMS studies of granitic rocks. In: Bouchez, J.L., Hutton, D.H.W., Stephens, W.E. (Eds.), Granite: From Segregation of Melts to Emplacement Fabric, Kluwer, Dordrecht, pp. 95-112.
Bouchez, J.L., Delas, C., Gleizes, G., Nedelec, A., Cuney, M., 1992. Submagmatic micro-fractures in granites. Geology 20 (1), 35-38.
Cruden, A.R., 1990. Flow and fabric development during the diapiric uprise of magma. Journal of Geology 98, 681-698.
Delaney, P.T., Pollard, D.D., Ziony, J.I., McKee, E.H., 1986. Field relations between dikes and joints: emplacement processes and paleostress analysis. Journal of Geophysical Research 91, 4920-4938.
Duchesne, J.C., 1973. Les gisements d'oxydes de fer et de titane dans les roches anorthositiques du Rogaland (Norvège méridionale). In: Morin, P., (Ed.), Les roches plutoniques dans leurs rapports avec les gÎtes minéraux, Masson, Paris, pp. 241-248.
Duchesne, J.C., 1996. Liquid ilmenite or liquidus ilmenite: a comment on the nature of ilmenite vein deposits. In: Demaiffe, D., (Ed.), Petrology and Geochemistry of Magmatic Suites of Rocks in the Continental and Oceanic Crusts, Université Libre de Bruxelles-Royal Museum for Central Africa (Tervuren), pp. 73-81.
Duchesne, J.C., 1999. Fe-Ti deposits in Rogaland anorthosites (South Norway): geochemical characteristics and problems of interpretation. Mineralium Deposita 34, 182-198.
Duchesne, J.C., Schiellerup, H., 2001. The iron-titanium deposits. In: Duchesne, J.C. (Ed.), The Rogaland Intrusive Massifs: an Excursion Guide. Norges geologiske undersøkelse Report 2001.029, pp. 57-78.
Duchesne, J.C., Maquil, R., Demaiffe, D., 1985. The Rogaland anorthosites: facts and speculations. In: Tobi, A.C., Touret, J.L.R. (Eds.), The Deep Proterozoic Crust in the North Atlantic Provinces, Reidel, Dordrecht, pp. 449-476.
Duchesne, J.C., Liegeois, J.P., Vander Auwera, J., Longhi, J., 1999. The crustal tongue melting model and the origin of massive anorthosites. Terra Nova 11, 100-105.
Dunlop, D.J., Özdemir, O., 1997. Rock Magnetism: Fundamentals and Frontiers, Cambridge University Press, Cambridge, 573pp.
Emslie, R.F., Hamilton, M.A., Thiérault, R.J., 1994. Petrogenesis of a Mid- Proterozoic Anorthosite-Mangerite-Charnockite- Granite (AMCG) complex: isotopic and chemical evidence from the Nain Plutonic Suite. Journal of Geology 102, 539-558.
Falkum, T., Petersen, J.S., 1980. The Sveconorwegian orogenic belt, a case of Late-Proterozoic plate-collision. Geologische Rundschau 69, 622-647.
Force, E.R., 1991. Geology of titanium mineral deposits. Geological Society of America Special Paper 259, 118.
Fueten, F., 1997. A computer controlled rotating polarizer stage for the petrographic microscope. Computers and Geosciences 23, 203-208.
Gierth, E., 1970. Die Ilmenitlagerstatte Tellnes (Süd-Norwegen). Ph.D. Thesis, T.U. Clausthal.
Gierth, E., Krause, H., 1973. Die Ilmenitlagerstätte Tellnes (Süd- Norwegen). Norsk Geologisk Tidsskrift, Supplement 53, 359-402.
Gierth, E., Krause, H., Schott, W., 1982. Paragenesen und Gefüge des hydrothermalen Nachhalls in südnorwegischen Titaneisenerzen. Erzmetall 35, 441-446.
Grégoire, V., Darrozes, J., Gaillot, P., Nedelec, A., Launeau, P., 1998. Magnetite grain shape fabric and distribution anisotropy vs. rock magnetic fabric: a three-dimensional case study. Journal of Structural Geology 7, 937-944.
Hargraves, R.B., Johnson, D., Chan, C.W., 1991. Distribution anisotropy: the cause of AMS in igneous rocks? Geophysical Research Letters 18, 2193-2196.
Hext, G.R., 1963. The estimation of second-order tensors, with related tests and design. Biometrika 50, 353-373.
Hoagland, R.G., Hahn, G.T., Rosenfield, A.R., 1973. Influence of microstructure on fracture propagation in rock. Rock Mechanics 5, 77-106.
Hunter, R.H., 1996. Texture development in cumulate rocks. In: Cawthorn, R.G., (Ed.), Layered Intrusions, Development in Petrology 15, Elsevier, Amsterdam, pp. 77-101.
Jackson, M., 1991. Anisotropy of magnetic remanence: a brief review of mineralogical sources, physical origins, and geological applications, and comparison with susceptibility anisotropy. Pure Applied Geophysics 136, 1-28.
Jackson, M., Gruber, W., Marvin, J., Banerjee, S.K., 1988. Partial anhysteretic remanence and its anisotropy: applications and grainsizedependence. Geophysical Research Letters 15, 440-443.
Jelinek, V., 1981. Characterization of the magnetic fabrics of rocks. Tectonophysics 79, 63-67.
Karlsen, T.A., Nilsson, L.P., Marker, M., Gautneb, H., Erichsen, E., 1998. Berggrunnsgeologi og mineralske ressurser i Sokndals-omr̊adet, Rogaland. Norges geologiske undersøkelse Report, 98068.
Krause, H., Pedall, K.G., 1980. Fe-Ti mineralizations in the Åna-Sira anorthosite, Southern Norway. In: Siivola, J. (Ed.), Metallogeny of the Baltic Shield. Finland Geological Survey Bulletin 307, pp. 56-83.
Krause, H., Gierth, E., Schott, W., 1985. Ti-Fe deposits in the South Rogaland igneous complex with special reference to the Åna- Sira anorthosite massif. Norges geologiske undersk̈else Bulletin 402, 25-37.
Lagroix, F., Borradaile, G.J., 2000. Magnetic fabric interpretation complicated by inclusions in mafic silicates. Tectonophysics 325, 207-225.
Launeau, P., Robin, P.Y.F., 1996. Fabric analysis using the intercept method. Tectonophysics 267, 91-119.
Launeau, P., Cruden, A.R., 1998. Magmatic fabric acquisition mechanisms in a syenite: results of a combined anisotropy of magnetic susceptibility and image analysis study. Journal of Geophysical Research 103, 5067-5089.
Longhi, J., Vander Auwera, J., Fram, M.S., Duchesne, J.C., 1999. Some phase equilibrium constraints on the origin of Proterozoic (massif) anorthosites and related rocks. Journal of Petrology 40, 339-362.
McLelland, J., Ashwal, L.D., Moore, L., 1994. Composition and petrogenesis of oxide-, apatite-rich gabbronorites associated with Proterozoic anorthosite massifs: example of the Adirondack mountains, New York. Contribution to Mineralogy and Petrology 116, 225-238.
Paterson, S.R., Vernon, R.H., Tobisch, O.T., 1989. A review of criteria for the identification of magmatic and tectonic foliations in granitoids. Journal of Structural Geology 11, 349-363.
Pollard, D.D., 1973. Derivation and evaluation of a mechanical model for sheet intrusions. Tectonophysics 19, 233-269.
Rochette, P., 1987. Magnetic susceptibility of the rock matrix related to magnetic fabric studies. Journal of Structural Geology 9, 1015-1020.
Rochette, P., Jackson, M., Aubourg, C., 1992. Rock magnetism and the interpretation of the anisotropy of magnetic susceptibility. Reviews of Geophysics 30, 209-226.
Schärer, U., Wilmart, E., Duchesne, J.C., 1996. The short duration and anorogenic character of anorthosite magmatism: U-Pb dating of the Rogaland Complex, Norway. Earth and Planetary Science Letters 139, 335-350.
Shimamoto, T., Ikeda, Y., 1976. A simple algebric method for strain estimation from deformed ellipsoidal objects. 1. Basic theory. Tectonophysics 36, 315-337.
Skjerlie, K.P., Kullerud, K., Robins, B., 2001. Preliminary melting experiments on the Tellnes ilmenite norite from 0.5 to 1.2 GPa, implications for the composition of intercumulus melt (abstract). In: Korneliussen, A. (Ed.), Abstracts-GEODE Field Workshop 8-12th July 2001 on Ilmenite Deposits in the Rogaland Anorthosite Province, S. Norway. Norges geologiske undersøkelse Report 2001.042, pp. 135- 136.
Smithson, S.B., Ramberg, I.B., 1979. Gravity interpretation of the Egersund anorthosite complex, Norway: its petrological and geothermal significance. Geological Society of America Bulletin 90, 199-204.
Stephenson, A., 1993. Three-axis static alternating field demagnetization of rocks and the identification of natural remanent magnetization, gyroremanent magnetization, and anisotropy. Journal of Geophysical Research 98, 373-381.
Streckeisen, A., 1974. How should charnockitic rocks be named? In: Duchesne, J.C., Bellière, J. (Eds.), Géologie des domaines cristallins, Volume du Centenaire de la Sociéte Géologique de Belgique, Liège, pp. 349-360.
Trindade, R.I.F., Bouchez, J.L., Bolle, O., Nedelec, A., Peschler, A., Poitrasson, F., 2001. Secondary fabrics revealed by remanence anisotropy: methodological analysis and examples from plutonic rocks. Geophysical Journal International 147, 310-318.
Uyeda, S., Fuller, M.D., Belsch, J.C., Girdler, R.W., 1963. Anisotropy of magnetic susceptibility of rocks and minerals. Journal of Geophysical Research 68, 279-291.
Vander Auwera, J., Duchesne, J.C., 1996. Petrology and geochemistry of the noritic Hogstad layered body (Rogaland, southwestern Norway): evidence for a jotunitic parent magma. In: Demaiffe, D., (Ed.), Petrology and Geochemistry of Magmatic Suites of Rocks in the Continental and Oceanic Crusts, U.L.B.-Royal Museum for Central Africa (Tervuren), pp. 111-127.
Vander Auwera, J., Longhi, J., 1994. Experimental study of a jotunite (hypersthene monzodiorite): constraints on the parent magma composition and crystallization conditions (P, T, fO2) of the Bjerkreim- Sokndal intrusion (Norway). Contributions to Mineralogy and Petrology 118, 60-78.
Vlag, P., Rochette, P., Dekkers, M.J., 1996. Some additional hysteresis parameters for a natural (titano)magnetite with known grain size. Geophysical Research Letters 23, 2803-2806.
Wilmart, E., Demaiffe, D., Duchesne, J.C., 1989. Geochemical constraints on the genesis of the Tellnes ilmenite deposit, Southwest Norway. Economic Geology 84, 1047-1056.