EÖTVÖS LORÁND TUDOMÁNYEGYETEM K ZETTANI ÉS GEOKÉMIAI TANSZÉK. Mikromineralógia

Átírás

1 EÖTVÖS LORÁND TUDOMÁNYEGYETEM K ZETTANI ÉS GEOKÉMIAI TANSZÉK Mikromineralógia Kiegészít ábraanyag a Mikromineralógia kurzus oktatási segédanyagához III. és IV. éves geológusok részére összeállította: Mikes Tamás, 2004

2 Morton & Hallsworth (1999) Hurst & Morton (2001)

3 Selley (2000) Törmelékes turmalinkristályok: Viator (2003), kissé módosítva

4 Johnsson (1993)

5 Morton & Hallsworth (1999) SAVAS MÉLY- ÁLTALÁNOS MÁLLÁS BETEMETÕDÉS STABILITÁSI SOR STABIL TiO 2 ásványok spinell, TiO 2 ásványok, TiO 2 ásványok INSTABIL Morton & Hallsworth (1999) alapján

6

7 monacit 4403 m krómspinell 3818 m gahnit 3016 m kloritoid 2728 m turmalin 4135 m turmalin 4135 m Morton & Hallsworth (1999)

8 gránát 1152 m gránát 1152 m gránát 2222 m gránát 2222 m gránát 2855 m gránát 2855 m Morton (1979)

9 gránát 2222 m gránát 3153 m gránát 3153 m staurolit 1152 m staurolit 1152 m staurolit 2222 m Morton (1979)

10 epidot 1152 m epidot 1487 m kianit 1152 m kianit 1487 m hornblende 1836 m apatit 2855 m Morton (1979)

11 augit hipersztén amfibol Morton (1984)

12 Morton & Hurst (1985)

13 Smale & Morton (1987)

14 Morton (1987)

15

16 Morton (1985b)

17 Haughton & Farrow (1984)

18 Boenigk (1983)

19 Haughton & Farrow (1984) Till (1992)

20 Hurst & Morton (2001) Ingersoll (1990)

21

22 Egyes cirkonkristályok morfológiája. a-e: mészalkáli k zetekb l (hibrid magmából) származó cirkon (a S23-as típus; b S24; c S24-25; d S19; e S17), f-j: kéregeredet cirkon (f S11; g S2; h L2; i S8; j S6), k-m: köpenyeredet cirkon (k P4; l P1; m P3), n-o: köpenyeredet, valószín leg tholeiites k zetekb l származó cirkon (n J4; o J5). A skála 10 µm hosszú. Mikes (2003), kissé módosítva

23 Mange-Rajetzky (1995)

24 Morton (1987)

25 Sabeen et al. (2002) Prp Prp SCA1 NW Istria RJA1 Brkini Basin ZBC1 Brkini Basin TAT1 Brkini Basin Alm Sps Mikes (2003)

26 von Eynatten et al. (1999) von Eynatten & Gaupp (1999)

27 Zack et al. (2002)

28 0 magnezioriebeckit ferroglaukofán riebeckit 0.2 Mg/(Mg+Fe ) Sesia-Lanzo Zóna (Tropper & Essene, 2002) Nilüfer egység, ÉNy Törökország (Okay et al., 2002) Fruška Gora, crossitpala (Milovanoviæ et al., 1995) Nyugati-Alpok (Bocquet, 1974) Vardar-öv és a Golija-öv (Majer & Lugoviæ, 1991) Meliaticum (Ájfalucskai Kékpala - Howie & Walsh, 1982) Savoy Molassz (Mange-Rajetzky & Oberhänsli, 1982) ÉNy Isztria / Trieszti-medence (Lenaz & Princivalle, 2002) ÉNy-Isztria (jelen munka) glaukofán VI Fe /(Fe + Al) Mikes (2003) Mange-Rajetzky (1981) Mange-Rajetzky & Oberhänsli (1982)

29 Spiegel et al. (2002)

30 Lee et al. (2003) von Eynatten & Gaupp (1999)

31 Felhasznált és ajánlott irodalom Lelőhelyek: ScienceDirect ( TTK Kari Könyvtár; Dr. Szakmány György; Mikes Tamás B. Árgyelán, G. (1996) Geochemical investigations of detrital chrome spinels as a tool to detect an ophiolitic source area (Gerecse Mountains, Hungary). Acta Geologica Hungarica, 39, Boenigk, W. (1983) Schwermineralanalyse. 158 p. Enke, Stuttgart. Caironi, V., Garzanti, E., and Sciunnach, D. (1996) Typology of detrital zircon as a key to unravelling provenance in rift siliciclastic sequences (Permo-Carboniferous of Spiti, N India). Geodinamica Acta, 9, Dunay, R.E. and Hailwood, E.A. (eds.) 1995: Non-biostratigraphical methods of dating and correlation, Geological Society Special Publication 89. Dunkl, I. (2002) Introduction to heavy mineral analysis and provenance studies. Compact course handout, Universität Tübingen, 43 p. Dunkl, I., Di Giulio, A., and Kuhlemann, J. (2001) Combination of single-grain fission-track chronology and morphological analysis of detrital zircon crystals in provenance studies - sources of the Macigno Formation (Apennines, Italy). Journal of Sedimentary Research, 71, Füchtbauer, H., Sediments and sedimentary rocks 1, Sedimentary Petrology (Part. 2): Stuttgart and New York (Schweiz. Verlagsbuch. and Halsted Press). Haughton, P.D.W., and Farrow, C.M. (1989) Compositional Variation in Lower Old Red Sandstone Detrital Garnets from the Midland Valley of Scotland and the Anglo-Welsh Basin. Geological Magazine, 126, Henry, D.J., and Dutrow, B.L. (1996) Metamorphic tourmaline and its petrologic applications. In L. Anovitz, and E. Grew, Eds. Boron: Mineralogy, petrology and geochemistry. Reviews in Mineralogy and Geochemistry 33, p Mineralogical Society of America. Henry, D.J., and Guidotti, C.V. (1985) Tourmaline as a petrogenetic indicator mineral: An example from the staurolitegrade metapelites of NW Maine. American Mineralogist, 70, Johnsson, M. J. (1993) The system controlling the composition of clastic sediments. In: Johnsson, M. J. and Basu, A. (eds.) 1993: Processes controlling the composition of clastic sediments, Geological Society of America, Special Paper 284, pp Johnsson, M. J. and Basu, A. (eds.) 1993: Processes controlling the composition of clastic sediments, Geological Society of America, Special Paper 284 Lee, J.I., Clift, P.D., Layne, G., Blum, J., and Khan, A.A. (2003) Sediment flux in the modern Indus River inferred from the trace element composition of detrital amphibole grains. Sedimentary Geology, 160, Lihou, J.C., and Mange-Rajetzky, M.A. (1996) Provenance of the Sardona Flysch, Eastern Swiss Alps: Example of highresolution heavy mineral analysis applied to an ultrastable assemblage. Sedimentary Geology, 105, Mange, M. A. and Maurer, H. F. W. (1992) Heavy Minerals in Colour. London: Chapman and Hall. Mange-Rajetzky, M.A. (1981) Detrital blue amphibole in recent sediments, southern coast, Turkey. Journal of the Geological Society, London, 138, Mange-Rajetzky, M. A. (1995) Subdivision and correlation of monotonous sandstone sequences using high-resolution heavy mineral analysis, a case study: the Triassic of the Central Graben. In: Dunay, R.E. and Hailwood, E.A. (eds.) 1995: Non-biostratigraphical methods of dating and correlation, Geological Society Special Publication 89, pp Mange-Rajetzky, M.A., and Oberhänsli, R. (1982) Detrital lawsonite and blue amphibole in the molasse of Savoy, France and their significance in assessing Alpine evolution. Schweizerische mineralogische und petrographische Mitteilungen, 62,

32 Mange-Rajetzky, M.A., and Oberhänsli, R. (1986) Detrital pumpellyite in the peri-alpine molasse. Journal of Sedimentary Petrology, 56, Mikes, T. (2003) A külső-dinári eocén flis lehordási területének mikromineralógiai vizsgálata. Diplomamunka, ELTE TTK Kőzettani és Geokémiai Tanszék, 78p. + függelék. Morton, A.C. (1979) Surface features of heavy mineral grains from Palaeocene sands of the Central North Sea. Scottish Journal of Geology, 15, Morton, A.C. (1984) Heavy minerals from Paleogene sediments, Deep Sea Drilling Project Leg 81: Their bearing on stratigraphy, sediment provenance and the evolution of the North Atlantic. Initial Reports of the Deep Sea Drilling Project, 81, Morton, A.C. (1985a) A new approach to provenance studies: Electron microprobe analysis of detrital garnets from Middle Jurassic sandstones of the North Sea. Sedimentology, 32, Morton, A.C. (1985b) Heavy minerals in provenance studies. In Zuffa, G. G. (ed.): Provenance of arenites, 148, p Reidel. Morton, A. C. & Hurst, A. (1995) Correlation of sandstones using heavy minerals: an example from the Statfjord Formation of the Snorre Field, northern North Sea. In: Dunay, R.E. and Hailwood, E.A. (eds.) 1995: Nonbiostratigraphical methods of dating and correlation, Geological Society Special Publication 89, pp Morton, A.C. (1987) Influences of provenance and diagenesis on detrital garnet suites in the Paleocene Forties Sandstone, Central North Sea. Journal of Sedimentary Petrology, 57, Morton, A.C., and Hallsworth, C.R. (1999) Processes controlling the composition of heavy mineral assemblages in sandstones. Sedimentary Geology, 124, Morton, A.C., Todd, S.P. and Haughton, P.D.W. (eds.) 1991: Developments in sedimentary provenance studies, Geological Society Special Publication 57. Pettijohn, F.J., Potter, P.E., and Siever, R. (1972) Sand and sandstone. 618 p. Springer, Berlin. Pupin, J.P. (1980) Zircon and granite petrology. Contributions to Mineralogy and Petrology, 73, Sabeen, H.M., Ramanujam, N., and Morton, A.C. (2002) The provenance of garnet: Constraints provided by studies of coastal sediments from southern india. Sedimentary Geology, 152, Smale, D., and Morton, A.C. (1987) Heavy mineral suites of core samples from the McKee formation (Eocene-Lower Oligocene), Taranaki: Implications for provenance and diagenesis. New Zealand Journal of Geology and Geophysics, 30, Spiegel, C., Siebel, W., Frisch, W., and Berner, Zs. (2002) Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators; implications for the reconstruction of the exhumation history of the Central Alps. Chemical Geology, 189, Till, A.B. (1992) Detrital blueschist-facies metamorphic mineral assemblages in Early Cretaceous sediments of the foreland basin of the Brooks Range, Alaska, and implications for orogenic evolution. Tectonics, 11, von Eynatten, H., and Gaupp, R. (1999) Provenance of Cretaceous synorogenic sandstones in the Eastern Alps: Constraints from framework petrography, heavy mineral analysis and mineral chemistry. Sedimentary Geology, 124, von Eynatten, H., Gaupp, R., and Wijbrans, J.R. (1996) 40 Ar/ 39 Ar laser-probe dating of detrital white micas from Cretaceous sedimentary rocks of the Eastern Alps: Evidence for Variscan high-pressure metamorphism and implications for Alpine orogeny. Geology, 24, Zack, T., Kronz, A., Foley, S.F., and Rivers, T. (2002) Trace element abundances in rutiles from eclogites and associated garnet mica schists. Chemical Geology, 184, Zuffa, G. G., Ed., Provenance of arenites, 148, p Reidel.