Quartz chemistry in polygeneration sveconorwegian pegmatites, Froland, Norway

European Journal of Mineralogy

Volumn 20, Issue 4, 2008, Pages 447-463

  Müller, Axel ^a   Ihlen, Peter M ^a   Kronz, Andreas ^b  

^a GEOLOGICAL SURVEY OF NORWAY   (Norway)

^b UNIVERSITY OF GÖTTINGEN   (Germany)

Author keywords

Cathodoluminescence; Froland; LA ICP MS; Pegmatite; Quartz; Trace elements

Indexed keywords

BIOTITE; CATHODOLUMINESCENCE; FELDSPAR; INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY; MASS SPECTROMETERS; MICA; QUARTZ; TRACE ELEMENTS;

AVERAGE CONCENTRATION; CHEMICAL VARIATIONS; CONTACT METAMORPHISM; ELEMENT CONCENTRATIONS; FROLAND; GRANITIC PEGMATITE; LA-ICP-MS; PEGMATITE;

GRANITE;

BIOTITE; CATHODOLUMINESCENCE; CHEMICAL ANALYSIS; CHEMICAL COMPOSITION; CONFERENCE PROCEEDING; FELDSPAR; GEOCHEMISTRY; MASS SPECTROMETRY; PEGMATITE; QUARTZ; TRACE ELEMENT;

AUST AGDER; EURASIA; EUROPE; FROLAND; NORTHERN EUROPE; NORWAY; SCANDINAVIA;

EID: 52049085033     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2008/0020-1822     Document Type: Conference Paper

References (75)

1. Abad-Ortega, M.D.M., Hach-Alí, P.F., Martin-Ramos, J.D., Ortega-Huertas, M. (1993): The feldspars of the Sierra Albarrana granitic pegmatites, Cordoba, Spain. Can. Mineral., 31, 185-202.
2. Alirezaei, S. (2000): Geochemical investigation of the lower crustal rocks in Bamble Shear belt, southern Norway: implications for the source of gold in lode gold deposits. Unpublished Ph.D. thesis, University of Ottawa, 343 p.
3. Ålmi R. (1975): Mineralogy and rare earth geochemistry of apatite and xenotime from the Gloserheia granite pegmatite, Froland, southern Norway. Am. Mineral., 60, 607-620.
4. Ålmi R. (1977): Internal structure and mineralogy of the Gloserheia granite pegmatite, Froland, southern Norway. Norsk Geol. Tidsskr., 57, 243-262.
5. Andersen, O. (1926): Feltspat I. Norges Geologiske Undersøkelse, 128a, 1-142. (in Norwegian)
6. Andersen, O. (1931): Feltspat II. Norges Geologiske Undersøkelse, 128b, 1-109 (in Norwegian).
7. Andersen, T. (1997): Radiogenic isotope systematics of the Herefoss Granite, South Norway; an indicator of Sveconorwegian (Grenvillian) crustal evolution in the Baltic Shield. Chem. Geol., 135, 139-158.
8. Andersen, T. (2005): Terrane analysis, regional nomenclature and crustal evolution in the Southwest Scandinavian Domain of the Fennoscandian Shield. GFF, 127, 159-168.
9. Andersen, T., Andresen, A., Sylvester, A.G. (2002): Timing of late-to post-tectonic Sveconorwegian granitic magmatism in South Norway. Norges Geol. Unders. Bull., 440, 5-18.
10. Baadsgaard, H., Chaplin, C., Griffin, W.L. (1984): Geochronology of the Gloserheia pegmatite, Froland, southern Norway. Norsk Geol. Tidsskr., 64, 111-119.
11. Behr, H.-J., Frentzel-Beyme, K. (1989): Permeability and pale-oporosity in crystalline bedrocks of the Central European basement-studies of cathodoluminescence. in "Exploration of the deep continental crust. Deep drilling in crystalline bedrock Volume 2." A. Boden, K.G. Eriksson, eds. Springer, Berlin Heidelberg New York, 477-497.
12. 39Ar geochronology across terrane boundaries in the Sveconorwegian Province of S. Norway. Precamb. Res., 90, 159-185.
13. Bingen, B., Nordgulen, Ø., Sigmund, E.M.O. (2001): Correlation of supracrustal sequences and origin of terranes in the Sveconorwegian orogen of SW Scandinavia: SIMS data on zircon clastic metasediments. Precamb. Res., 108, 293-318.
14. Bingen, B., Mansfeld, J., Sigmond, E.M.O., Stein, H. (2002): Baltica-Laurentia link during the Mesoproterozoic: 1.27 Ga development of continental basins in the Sveconorwegian orogen, South Norway. Can. J. Earth Sci., 39, 1425-1440.
15. Bjørlykke, H. (1937): The granite pegmatites of southern Norway. Am. Mineral., 22, 241-255.
16. Botis, S., Nokhrin, S.M., Pan, Y., Xu, Y., Bonli, T. (2005): Natural radiation-induced damage in quartz. I. Correlations between cathodoluminescence colors and paramagnetic defects. Can. Mineral., 43, 1565-1580.
17. Brøgger, W.C. (1906) Die Mineralien der südnorwegischen Granitpegmatitgänge. Videnskaps-Selskape i Christiana, 1/6, 1-162.
18. Cameron, E.N., Jahns, R.H., McNair, A.H., Page, L.R. (1949): Internal structure of granitic pegmatites. Econ. Geol. Monogr., 2, 115 p.
19. Çerný, P. (1992): Regional zoning of pegmatite populations and its interpretation. Mitt. Österr. Mineral. Ges., 137, 99-107.
20. Çerný, P. & Burt, D.M. (1984): Paragensis, crystallochemical properties, and chemical evolution of micas in granite pegmatites. in "Micas" S.W. Bailey, ed., Reviews in Mineralogy, 13, 257-297.
21. Çerný P. & Ercit, T.S. (2005): The classification of granitic pegmatites. Can. Mineral., 43, 2005-2026.
22. Chakoumakos, B.C. & Lumpkin, G.R. (1990): Pressure-temperature constraints on the crystallization of the Harding pegmatite, Taos County, New Mexico. Can. Mineral., 28, 287-298.
23. Cosca, M.A., Mezger, K., Essene, E.J. (1998): The Baltica-Laurentia connection: Sveconorwegian (Grenvillian) metamorphism, cooling, and unroofing in the Bamble sector, Norway. J. Geology, 106, 539-552.
24. Cox, R.A., Dempster T.Y., Bell B.R., Rogers, G. (1996): Crystallization of the Shap Granite: Evidence from zoned K-feldspar megacrysts. J. Geol. Soc. London, 153, 625-635.
25. Elders, W.A. (1963): On the form and mode of emplacement of the Herefoss granite. Norwegian Geol. Surv. Bull., 214, 1-50.
26. Flem, B., Larsen, R.B., Grimstvedt, A., Mansfeld, J. (2002): In situ analysis of trace elements in quartz by using laser ablation inductively coupled plasma mass spectrometry. Chem. Geol., 182, 237-247. Götze, J., Plötze, M., Habermann, D. (2001): Origin, spectral characteristics and practical applications of the cathodoluminescence (CL) of quartz - a review. Mineral. Petrol., 71, 225-250.
27. Götze, J., Plötze, M., Graupner, T., Hallbauer, D.K., Bray, C.J. (2004): Trace element incorporation into quartz: A combined study by ICP-MS, electron spin resonance, cathodoluminescence, capillary ion analysis, and gas chromatography. Geochim. Cosmochim. Acta, 68, 3741-3759.
28. Götze, J., Plötze, M., Trautmann, T. (2005): Structure and luminescence characteristics of quartz from pegmatites. Am. Mineral., 90, 13-21.
29. Harben, P.W. (2002): The industrial mineral handybook - a guide to markets, specifications and prices. 4th edition, Industrial Mineral Information, Worcester Park, United Kingdom, 412 p.
30. 2 diffusion in hydrous siliceous melts. EOS (Transactions, American Geophysical Union), v. 86, Fall meeting supplement, abs. MR13A-0076.
31. Henderson, I. (2002): CL mikroteksturer i tilknytning til polypfase kvarts i pegmatitter i Frolandsområde. in "Potensielle ressurser av kvarts- og feldspat- råstoffer på Sørlandet, II: Resultater av undersøkelsene i Frolandsområdet i 2001" P.M. Ihlen, I. Henderson, R.B. Larsen, R. Lynum eds., Norwegian Geological Survey Report 2002.009, Trondheim, 65-72 (in Norwegian).
32. Henderson, I. & Ihlen, P.M. (2004): Emplacement of polygeneration pegmatites in relation to Sveco-Norwegian contractional tectonics: examples from southern Norway. Precamb. Res., 133, 207-222.
33. Ihlen, P.M. & Müller, A. (2007): Hydrothermal formation of high-purity quartz deposits along the Hardangerfjord Fault Zone. NGF Abstracts and Proceedings of the Geological Society of Norway, Stavanger, 8-10. January 2007, 1, 46-47.
34. Ihlen, P.M., Lynum, R., Henderson, I., Larsen, R.B. (2001): Potensielle ressurser av kvarts- og feldspat- råstoffer på Sørlandet, I: Regional prøvetaking av utvalgte feltspatbrudd i Frolandsområdet. Norwegian Geological Survey Report 2001.044, Trondheim, 46 p. (in Norwegian).
35. Ihlen, P.M., Henderson, I., Larsen, R.B., Lynum, R. (2002): Potensielle ressurser av kvarts- og feldspat- råstoffer på Sørlandet, II: Resultater av undersøkelsene i Frolandsområdet i 2001. Norwegian Geological Survey Report 2002.009, Trondheim, 100 p. (in Norwegian).
36. Jacamon, E & Larsen, R.B. (2006): Trace element evolution in quartz during fractional crystallisation of the high T and P charnockitic Kleivan granite, south-western Norway. in "The significance of textures and trace element chemistry of quartz with regard to the petrogenesis of granitic rocks", E Jacamon, PhD thesis, NTNU Norwegian University of Science and Technology, Trondheim, 1-34.
37. Knudsen, T.-L. & Andersen, T. (1999): Petrology and geochemistry of the Tromoy gneiss complex, South Norway, an alleged example of Proterozoic depleted lower continental crust. J. Petrol., 40, 909-933.
38. Larsen, R.B. (2002): The distribution of rare-earth elements in K-feldspars as an indicator of petrogenetic processes in granitic pegmatites: Examples from two pegmatite fields in southern Norway. Can. Mineral., 40, 137-151.
39. Larsen, R.B., Henderson, I., Ihlen, P.M., Jacamon, F. (2004): Distribution and petrogenetic behaviour of trace elements in granitic quartz from South Norway. Contrib. Mineral. Petrol., 147, 615-628.
40. London, D. (1996): Granitic pegmatites. Trans. Royal Soc. Edinburgh, 87, 305-319.
41. London, D. (2005): Granitic pegmatites: an assessment of current concepts and directions for the future. Lithos, 80, 281-303.
42. 2O, at 200 MPa, and the internal differentiation of granitic pegmatites. Contrib. Mineral. Petrol., 102, 1-17.
43. Long, P.E. & Luth, W.C. (1986): Origin of K-feldspar megacrysts in granitic rocks: Implication of a partitioning model for barium. Am. Mineral., 71, 367-375.
44. Malló, A., Fontan, F., Melgarejo, J. C., Mata, J. M. (1995): The Albera zoned pegmatite field, Eastern Pyrenees, France. J. Mineral. Petrol., 55, 103-116.
45. Mehnert, K.R. & Büsch, W. (1981): The Ba content of K-feldspar megacrysts in granites: a criterion for their formation. N. Jb. Miner. Abh., 140, 221-252.
46. Morgan, G.B. & London, D. (1999): Crystallization of the Little Three layered pegmatite-aplite dike, Ramona District, California. Contrib. Mineral. Petrol., 136, 310-330.
47. Müller, A., Seltmann, R., Behr, H.J. (2000): Application of cathodoluminescence to magmatic quartz in a tin granite - case study from the Schellerhau Granite Complex, Eastern Erzgebirge, Germany. Mineral. Deposita, 35, 169-189.
48. Müller, A., Kronz, A., Breiter, K. (2002a): Trace elements and growth patterns in quartz: a fingerprint of the evolution of the subvolcanic Podlesí Granite System (Krugne Hory, Czech Republic). Bull. Czech Geol. Surv., 77/2, 135-145.
49. Müller, A., Lennox, P., Trzebski, R. (2002b): Cathodoluminescence and micro-structural evidence for crystallisation and deformation processes of granites in the Eastern Lachlan Fold Belt (SE Australia). Contrib. Mineral. Petrol., 143, 510-524.
50. Müller, A., Rene, M., Behr, H.-J., Kronz, A. (2003a): Trace elements and cathodoluminescence of igneous quartz in topaz granites from the Hub Stock (Slavkovský Les Mts., Czech Republic). Mineral. Petrol., 79, 167-191.
51. Müller, A., Wiedenbeck, M., van den Kerkhof, A.M., Kronz, A., Simon, K. (2003b): Trace elements in quartz - a combined electron microprobe, secondary ion mass spectrometry, laser-ablation ICP-MS, and cathodoluminescence study. Eur. J. Mineral., 15, 747-763.
52. Müller, A., Ihlen, P.M., Kronz, A. (2005): Potential resources of quartz and feldspar raw material in Sørland IV: Relationships between quartz, feldspar and mica chemistry and pegmatite type. Norwegian Geological Survey Report 2005.075, Trondheim, 94 p.
53. Nijland, T.G., Maijer, C. (1993): The regional amphibolite to granulite facies transition at Arendal, Norway: Evidence for a thermal dome. N. Jb. Miner Abh., 165, 191-221.
54. Norton, J.J. (1983): Sequence of mineral assemblages in differentiated granitic pegmatites. Econ. Geol., 78, 854-874.
55. Perny, B., Eberhardt, P., Ramseyer, K., Mullis, J., Pankrath, R. (1992): Microdistribution of aluminium, lithium and sodium in a quartz: possible causes and correlation with shored lived cathodoluminescence. Am. Mineral., 77, 534-544.
56. Ramseyer, K., Baumann, J., Matter, A., Mullis, J. (1988): Cathodoluminescence, colours of α-quartz. Mineral. Mag., 52, 669-677.
57. Roda-Robles, E., Pesquera, A., Gil, P. P., Torres-Ruiz, J., Fontan, F. (2004): Tourmaline from the rare-element Pinilla pegmatite, (Central Iberian Zone, Zamora, Spain): chemical variation and implications for pegmatitic evolution. J. Mineral. Petrol., 81, 249-263.
58. Schetelig, J. (1922): Thortveitite. Nor. Geol. Tidsskr,. 6, 233-243.
59. Schrön, W., Schmädicke, E., Thomas, R., Schmidt, W. (1988): Geochemische Untersuchungen an Pegmatitquarzen. Z. geol. Wiss., 16, 229-244.
60. Shearer, C.K., Papike, J.J., Jolliff, B.L. (1992): Petrogenetic links amoung granites and pegmatites in the Harney Peak rare-element granitic pegmatite system, Black Hills, South Dakota. Can. Mineral., 30, 785-809.
61. Sprunt, E.S. (1981): Causes of quartz cathodoluminescence colors. Scanning Electron Microscopy, 1981, 525-535.
62. Sprunt, E.S. & Nur, A. (1979): Microcracking and healing in granites: New evidence from cathodoluminescence. Science, 205, 495-497.
63. Starmer, I.C. (1993): The Sveconorwegian Orogeny in Southern Norway, relative to deep crustal structures and eventsin the North Atlantic Proterozoic supercontinent. Norsk Geol. Tidsskr., 73, 109-132.
64. Stenina, N.G., Bazarov, L.S., Shcherbakova, M.Y., Mashkovtsev R.I., 1984. Structural state and diffusion of impurities in natural quartz of different genesis. Phys. Chem. Minerals 10, 180-186.
65. Stevens Kalceff, M.A., Phillips, M.R., Moon, A.R., Kalceff, W. (2000): Cathodoluminescence microcharacterization of silicon dioxide polymorphs. in "Cathodoluminescence in Geosciences" M. Pagel, V. Barbin, P. Blanc, D. Ohnenstetter, eds. Springer, Berlin, 193-279.
66. Tischendorf, G., Förster, H.J., Gottesmann, B. (2001): Minor- and trace-element composition of trioctahedral micas: a review. Mineral Mag., 65, 249-276.
67. Touret, J. (1971a): Lafacies granulite en Norvege meridionale. I Les associations minéralogiques. Lithos, 4, 239-249.
68. Touret, J. (1971b): La facies granulite en Norvege meridionale. II Les inclusions fluides. Lithos, 4, 423-436.
69. Van den Kerkhof, A.M. & Hein, U. (2001): Fluid inclusion petrography. Lithos, 55, 27-47.
70. Van den Kerkhof, A.M., Kronz, A., Simon, K. (2001): Trace element redistribution in metamorphic quartz and fluid inclusion modification: observations by cathodoluminescence. XVI ECROFI, Porto 2001, Departomento Geologica Memória, 7, 447-450.
71. Van den Kerkhof, A.M., Kronz, A., Simon, K., Scherer, T. (2004): Fluid-controlled quartz recovery in granulite as revealed by cathodoluminescence and trace element analysis (Bamble sector, Norway). Contrib. Mineral. Petrol., 146, 637-652.
72. Vollbrecht, A., Rust, S., Weber, K. (1991): Development of microcracks in granites during cooling and uplift: examples from the Variscan basement in NE Bavaria, Germany. J. Struct. Geol., 13, 787-799.
73. Vollbrecht, A., Olesen, N.O., Schmidt, N.H., Weber, K. (1994): Crystallographic microcrack orientation in quartz from a granite - a combined ECP/U stage study. in "Textures of Geological Materials", H.J. Bunge, S. Siegesmund, W. Skrotzki, K. Weber, eds. DGM Informationsgeselischaft Verlag, Oberursel, 345-352.
74. Wark, D.A. & Watson, E.B. (2006): TitaniQ: a titanium-in-quartz geothermometer. Contrib. Mineral. Petrol., 152, 743-754.
75. Webber, K.L., Simmons, W.B., Falster, A.U., Foord, E.E. (1999): Cooling rates and crystallization dynamics of shallow level pegmatite-aplite dikes, San Diego County, California. Am. Mineral., 84, 708-717.