Advantages and limitations of interpretations of external morphology of detrital zircon: a case study of the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpathians)

Salata, D.

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Advantages and limitations of interpretations of external morphology of detrital zircon: a case study of the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpathians)

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Salata D.

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Abstrakty

The zircon populations from the Campanian–Maastrichtian part of the Ropianka (Upper Cretaceous– Palaeocene) and Menilite (Oligocene–lower Miocene) formations in the northern part of the Skole Nappe in Poland were examined to evaluate interpretations of the external morphology of detrital zircon in provenance research. The advantage of the zircon typology method, supplemented with elongation measurements, is that it may be applied successfully to comparisons of euhedral zircon populations from sedimentary deposits of different ages and unknown provenance. The zircon typology method, along with elongation measurements of zircons, contributes valuable data that supplement conventional heavy-mineral analyses. It also permits the recognition of potential source areas and rock types for further comparative research.

Słowa kluczowe

detrital zircon morphology flysch Skole Nappe Outer Carpathians

Wydawca

Polskie Towarzystwo Geologiczne

Czasopismo

Annales Societatis Geologorum Poloniae

Rocznik

2014

Tom

Vol. 84, No. 2

Strony

153--165

Opis fizyczny

Bibliogr. 67 poz., rys.

Twórcy

autor

Salata D.

dorota.salata@uj.edu.pl

Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland

Bibliografia

1. Benisek, A. & Finger, F., 1993. Faciors conirolhng the development of prism faces in granite zircons: A microprobe study. Contributions to Mineralogy and Petrology, 114: 441-451.
2. Bromowicz, J., 1974. Facial variability and lithological character of Inoceramian Beds of the Skole Nappe beiween Rzeszów and Przemyśl. Prace Geologiczne, 84: 1-81. [In Polish, with English summary.]
3. Bromowicz, J., 1986. Petrographic differentiation of source areas of Ropianka Beds east of Dunajec River (Outer Carpathians, Poland). Annales Societatis Geologorum Poloniae, 56: 253276. [In Polish, with English summary.]
4. Bukowy, S., 1957. Remarks on the sedimentation of the Babica Clays. Rocznik Polskiego Towarzystwa Geologicznego, 26: 147-155. [In Polish, with English summary.]
5. Buła, Z., Jachowicz, M. & Żaba, J., 1997. Principal characteristics of the Upper Silesian Block and Małopolska Block border zone (southern Poland). GeologicalMagazine, 134: 669-677.
6. Caironi, V., Colombo, A., Tunesi, A. & Gritti, C., 2000. Chemical variation of zircon compared with morphological evolution during magmatic crystallization: an example from the Valle del Cervo Pluton Western Alps). European Journal of Mineralogy, 12: 779-794.
7. Caironi, V., Garzanti, E. & Sciunnach, D., 1996. Typology of detrilal zircon as a key to unravelling provenance in rift siliciclastic sequences (Permo-Carbonlferous of Spiti, N India). Geodinamica Acta, 9: 101-113.
8. Corfu, F., Hanchar, J. M. & Kinny, P., 2003. Atlas of zircon textures. In: Hanchar, J. M. & Hoskin P. W. O. (eds), Zircon. Reviews in Mineralogy and Geochemistry, 53: 468-500.
9. Czerny, J. & Muszyński, M., 1997. Co-magmatism of the Permian volcanites of the Krzeszowice area in the light of petrochemical data. Mineralogia Polonica, 28: 3-25.
10. El Baghdadi, M., El Boukhari, A., Jouider, A., Benyoucef, A. & Nadem, S., 2003. Calc-alkaline arc I-type granitoid assocf ated with S-type granite in the Pan-Aflican belt of eastern Anti-Atlas (Saghro and Ougnat, South Morocco). Gondwana Research, 6: 557-572.
11. Eynaten, H, von, & Dunkl, I., 2012. Assessing the sediment factory: The role of single grain analylis. Earth-Science Reviews, 115: 97-120.
12. Fekkak, A., Boualou, M., Badr, L., Amenzo, M., Saquaqu, A. & El-Amran I.E., 2000. Origin and geotectonic setting of lower Neoproterozoic Kelaat Mgouna detrital material (eastern Anti-Atlas, Morocco). Journal ofAfrican Earth Sciences, 30: 295-311.
13. Gasiński, M. A. & Uchman, A., 2009. Latest Maastrichtian fora- miniferal assemblages from the Husów region (Skole Nappe, Outer Carpathians, Poland). Geologica Carpathica, 60: 283294.
14. Gucwa, I. & Pelczar, A., 1992. Katalog analiz chemicznych skal Karpat polskich za lata 1963-1985. Cz.2 Skaly magmowe i metamorficzne. Państwowy Instytut Geologiczny, Warszawa, 132 pp. [In Polish.]
15. Harańczyk, C., 1989. Wulkanizm rejonu Krzeszowic. In: Rutkowski J. (ed.), Rozwój wulkanizmu krakowskiego. Przewodnik LX Zjazdu PTG, Kraków 14-15 września 1989: Wydawnictwa AGH, Państwowy Instytut Geologiczny, Kraków, pp. 51-58. [In Polish.]
16. Jasionowicz, J. & Wieser, T., 1963. O występowaniu bloków skał wulkanicznych w osadach fliszowych okolic Ropczyc. Kwartalnik Geologiczny, 7: 712-713. [In Polish.]
17. Kotlarczyk, J., 1966. Diatomite horizon of the Krosno Beds in the Skole Nappe, Polish Carpathians. Studia Geologica Polonica, 19: 110-129. [In Polish, with English summary.]
18. Kotlarczyk, J., 1976. Przyczynki do wyjaśnienia genezy piaskowców kliwskich w Karpatach Polskich. Sprawozdania z Posiedzeń Komisji Naukowej PAN, Oddzial Kraków, 19: 185-187. [In Polish.]
19. Kotlarczyk, J., 1978. Stratigraphy of the Ropianka Formation or of Inoceramian beds in the Skole Unit of the Flysch Carpathians. Prace Geologiczne, 108: 1-81. [In Polish, with English summary.]
20. Kotlarczyk, J. & Leśniak, T., 1990. Lower part of the Menilite Formation and Related Futoma Diatomite Member in the Skole Unit of the Polish Carpathians. Wydawnictwo Akademii Górniczo-Hutniczej, Kraków, 74 pp. [In Polish, with English summary.]
21. Kotlarczyk, J. & Śliwowa, M., 1963. On knowledge of the productive Carboniferous formations in the substratum of the eastern part of the Polish Carpathians. Przegląd Geologiczny, 11: 268-272. [In Polish, with English summary.]
22. Köksal, S., Cemal Göncüoglu, M., Toksoy-Köksal, F., Möller, A. & Kemnitz, H., 2008. Zircon typologies and internal structures as petrogenetic indicators in contrasting granitoid types from cenlral Anatolia, Turkey. Mineralogy and Petrology, 93: 185-211.
23. Książkiewicz, M. (ed.), 1962. Geological Atlas of Poland. Fascicle 13 - Cretaceous and Early Tertiary in the Polish External Carpathians. Instytut Geologiczny, Warszawa.
24. Lewandowska, A., Rospondek, M. J. & Nawrocki, J., 2010. Stephanian-Early Permian basaltic trachyandesites from the Sławków and Nieporaz-Brodła grabens near Kraków, Southern Poland. Annales Societatis Geologorum Poloniae, 80: 227-251.
25. Lihou, J. C. & Mange-Rajetzky, M. A., 1996. Provenance of the Sardona Flysch, eastern Swiss Alps: example of high-resolution heavy mineral analysis applied to an ultrastable assemblage. Sedimentary Geology, 105: 141-157.
26. Lisá, L. & Uher, P., 2006. Provenance of Würmian loess and loess-like sedlments of Moravia and Silesia (Czech Republic): A study of zircon typology and cathodoluminiscence. Geologica Carpathica, 57: 397-403.
27. Loi, A. & Dabard, M. P., 1997. Zircon typology and geochemistry in the palaeogeographic reconstruct ion of the Late Ordovician of Sardinia (Italy). Sedimentary Geology, 112: 263-297.
28. Malata, T., 1996. Analysis of standard lithostratigraphic nomenclat ure and proposal of division of Skole Unit in the Polish Flysch Carpathians. Geological Quarterly, 40: 543-554.
29. Malinowski, M., Żelaźniewicz, A., Grad, M., Guterch, A. & Janik, T., 2005. Seismic and geological structure of the crust in the transition from Baltica to Palaeozoic Europe in SE Poland - CELEBRATION 2000 experiment, profile CEL02. Tectonophysics, 401 : 55-77.
30. Mange, M. A. & Wright, D. T. (eds), 2007a. Heavy Minerals in Use. Developments in Sedimentology, 58, 1283 pp.
31. Mange, M. A. & Wright, D. T., 2007b. High-Resolulion Heavy Mineral Analysis (HRHMA): A Brief Summary. In: Mange, M. A. & Wright, D. T. (eds), Heavy Minerals in Use. Developments in Sedimentology, 58: 433-436. Elsevier, Amsterdam.
32. Mange-Rajetzky, M. A., 1995. Subdivision and correlation of monotonous sandstone sequences using high resolution heavy mineral analysis, a case study: the Triaslic of the Central Graben. Geological Society Special Publications, 89: 23-30.
33. Morlon, A. C. & Hallsworth, C. R., 1999. Processes conlrolling the composition of heavy mineral assemblages in sandstones. Sedimentary Geology, 124: 3-29.
34. Morlon, A. C. & Hallsworth, C. R., 2007. Stability of delrilal heavy minerals during burial diagenesis. In: Mange, M. A. & Wright, D. T. (eds), Heavy Minerals in Use. Developments in Sedimentology, 58: 215-245.
35. Nawrocki, J., Krzemiński, L. & Pańczyk, M., 20 1 0. 40Ar-39Ar ages of sel ected rocks and minerals from the Kraków-Lubliniec Fault Zone, and their relation to the Paleozoic structural evolulion of the Małopolska and Brunovistulian terrranes (S Poland). Geological Quarterly, 54: 289-300.
36. Nehyba, S., Roetzel, R. & Maštera, L., 2012. Provenance analysis of the Permo-Carbonlferous fluvial sandstones of the southern part of the Boskovice Basin and the Zöbing Area (Czech Republic, Austria): Implications for paleogeographical reconstructions of the post-Variscan collapse baslns. Geologica Carpathica, 63: 365-382.
37. Nie, J., Horlon, B. K., Saylor, J. E., Mora, A., Mange, M., Garzione, C. N., Basu, A., Moreno, C. J., Caballero, V. & Parra, M., 2012. Integrated provenance analysis of a convergent retroarc foreland system: U-Pb ages, heavy minerals, Nd isotopes, and sandstone compositions of the Middle Magdalena Valley basin, northern Andes, Colombia. Earth-Science Reviews, 110: 111-126.
38. Oszczypko, N., Ślączka, A. & Żytko, K., 2008. Tectonic subdivision of Poland: Polish Outer Carpathians and their foredeep. Przegląd Geologiczny, 56: 927-935. [In Polish, with English abstract.]
39. Pietsch, K., Golonka, J., Marzec, P. & Florek, R., 2010. Structural inierpreiaiion of seismic data in Polish Outer Carpathians south west and south east of Krakow. Scientific Annals, School of Geology, Aristotle University of Thessaloniki, Proceedings of the XIX CBGA Congress, Thessaloniki, Greece, 99: 21-29.
40. Poprawa, P., Malata, T., Pécskay, Z., Kusiak, M. A., Banaś, M. & Paszkowski, M., 2006. Geochronology of the crysialline basement of the Western Outer Carpathians’ source areas - constraints from K/Ar dating of mica and Th-U-Pb chemical dating of monazite from the crysianine ‘exotic’ pebbles. Geolines, 20: 110-112.
41. Pupin, J. P., 1980. Zircon and granite petrology. Contributions to Mineralogy and Petrology, 73: 207-220.
42. Pupin, J. P., 1988. Granites as indicaiors in palaeogeodynamics. Rendiconti della Societa Italiana di Mineralogia a Petrologia, 43: 237-262.
43. Rajchel, J., 1990. Lithostratigraphy of the Upper Paleocene and Eocene sediments from the Skole Unit. Zeszyty Naukowe AGH, Geologia, 48: 1-112. [In Polish, with English summary.]
44. Rajchel, J. & Myszkowska, J., 1998. Exotic clasts of organodetritic algal limestones from lithosomes of the Babica Clay, Skole Unit (Outer Flysch Carpathians, Poland). Annales So- cietatis Geologorum Poloniae, 68: 225-235.
45. Salata, D., 2013a. Source rocks for heavy minerals in lower part of Menilite Formation of Skole Nappe (Polish Flysch Carpathians), based on study of deirital garnet and tourmaiine. Annales Societatis Geologorum Poloniae, 83: 1-17.
46. Salata, D., 2013b. Garnet provenance in mixed first-cycle and poly-cycle heavy-mineral assemblages of the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpa- thians): constraints from chemical composition and grain morphology. Annales Societatis Geologorum Poloniae, 83: 161-177.
47. Salata, D., 2014. Detrital tourmaline as an indicator of source rock lithology: an example from the Ropianka and Menilite formations (Skole Nappe, Polish Flysch Carpathians). Geological Quarterly, 58: 19-30.
48. Salata, D. & Uchman, A., 2012. Heavy minerals from the Oligocene sandstones of the Menilite Formation of the Skole Nappe, SE Poland: a tool for provenance specification. Geological Quarterly, 56: 803-820.
49. Salata, D. & Uchman, A., 2013. Conventional and high-resolution heavy mineral analyses applied to flysch sediments: comparative provenance studies of the Ropianka (Upper Cretaceous- Palaeocene) and Menilite (Oligocene) formations (Skole Nappe, Polish Carpathians). Geological Quarterly, 57: 649664.
50. Schöfer, J. & Dörr, W., 1997. Heavy-mineral analysis and typology of deiriial zircons; a new approach to provenance study (Saxothuringian flysch, Germany). Journal of Sedimentary Research, 67: 451-461.
51. Shahbazi, H., Saiami, S. & Siebel, W., 2014. Genetic classification of magmatic rocks from the Alvand plutonic complex, Hamedan, western Iran, based on zircon crystal morphology. Chemie der Erde - Geochemistry, (in press).
52. Słaby, E., Breitkreuz, C., Żaba, J., Domańska-Siuda, J., Gadzik, K., Falenty, K. & Falenty, A., 2010. Magma generation in an alternating transtensional-transpressional regime, the Kraków-Lubliniec Fault Zone, Poland. Lithos, 119: 251-268.
53. Sturm, R., 1999. Factors controlling the pyramidal growth of zircon: new results. Neues Jahrbuch für Mineralogie, Monatshefte, 11: 494-504.
54. Sturm, R., 2010. Morphology and growth trends of accessory zircons from various granitoids of the South-western Bohemian Massif (Moldanubicum, Austria). Chemie der Erde, 70: 185196.
55. Szczepanik, P., 2001. Minerały akcesoryczne i biotyty w porfirach z Zalasu. Unpublished MSc. Thesis, Jagiellonian University, 146 pp. [In Polish.]
56. Ślączka, A. & Unrug, R., 1966. Sedimentary structures and petrology of some sandstone members of the Menilite Beds, Carpathians. Rocznik Polskiego Towarzystwa Geologicznego, 36: 155-184. [In Polish, with English summary.]
57. Vavra, G., 1990. On the kinematics of zircon growth and its petrogenetic significance: A cathodoluminescence study. Contributions to Mineralogy and Petrology, 106: 90-99.
58. Vavra, G., 1993. A guide to quantitative morphology of accessory zircon. Chemical Geology, 110: 15-28.
59. Wdowiarz, S., 1949. Struciure géologique des Carpates marginales au sudest de Rzeszów. Biuletyn Państwowego Instytutu Geologicznego, 11: 1-51. [In Polish, with French summary.]
60. Willner, A. P., Sindern, S., Metzger, R., Ermolaeva, T., Kramm, U., Puchkov, V. & Kronz, A., 2003. Typology and single grain U/Pb ages of detrital zircons from Proterozoic sandistones in the SW Urals (Russia): early time marks at the eastern margin of Baltica. Precambrian Research, 124: 1-20.
61. Wilson, M., 1989. Igneous Petrogenesis. Chapman&Hall, 466 pp.
62. Winchester, J. A. & the PACE TMR Network Team, 2002. Paleozoic amalgamation of Central Europe: new results from recent geological and geophysical investigations. Tectonophysics, 360: 5-21.
63. Wolska, A., 2012. Petrology and geochemásiry of granitoids and their mafic microgranular enclaves (MME) in marginal part of the Małopolska Block (S Poland). Mineralogia, 43: 3-127.
64. Zajzon, N., Szabö, Z., Weiszburg, T. G. & Jeffries, T. E., 2011. Multiple provenance of detrital zircons from the Permian- Triassic boundary in the Bükk Mts., Hungary. International Journal of Earth Sciences, 100: 125-138.
65. Żaba, J., 1999. Structural evoiution of Lower Palaeozoic succession in the Upper Silesia block and Małopolska block zone. Prace Państwowego Instytutu Geologicznego, 166: 5-162.
66. Żelaźniewicz, A., Pańczyk, M., Nawrocki, J. & Fanning, M., 2008. A Carboniferous/Permian, calc-alkaline, I-type granodiorite from the Małopolska Block, southern Poland: implications from geochemical and U-Pb zircon age data. Geological Quarterly, 52: 301-308.
67. Żgiet, J., 1963. Wstępna charakterystyka sedymentologiczna piaskowców kliwskich. Kwartalnik Geologiczny, 7: 715-716. [In Polish.]

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