The tectonometamorphic evolution of the marbles in the Lądek-Śnieżnik Metamorphic Unit, West Sudetes

Jastrzębski, M.

Artykuł - szczegóły

Tytuł artykułu

The tectonometamorphic evolution of the marbles in the Lądek-Śnieżnik Metamorphic Unit, West Sudetes

Autorzy

Jastrzębski M.

Wybrane pełne teksty z tego czasopisma

http://geojournals.pgi.gov.pl/gs/index

Identyfikatory

Warianty tytułu

Języki publikacji

Abstrakty

Together with the adjacent rocks, the marbles of the Lądek-Śnieżnik Metamorphic Unit (LSMU), West Sudetes, SW Poland underwent a polyphase structural evolution that occurred in metamorphic conditions changing from medium-grade to low-grade and in deformation regimes changing from ductile to semi-brittle. The structural evolution of the marbles began with E-W subhorizontal shortening resulting in the tilting of the Cal-Dol layering (which had generally originated as a pre-tectonic and pre-metamorphic feature) and its transposition to a steeply dipping metamorphic S1 foliation. The subsequent vertical flattening occurred at the temperature peak of regional metamorphism and produced the N-S trending tight, recumbent F2 folds. This event is also documented by the subhorizontal S2 axial-plane carbonate grain shape fabric and the parallel alignment of Phl-MsšTršCzo in the marbles, and the S2 axial-plane schistosity in the adjacent mica schists. The temperature increase was associated with the progressive mineral sequence Phl › Tr › Di in the dolomite-bearing marbles, which probably initially equilibrated at low to moderate X(CO2). Under peak temperatures, the observed arrangement of the metamorphic zonation of the Stronie formation developed, overprinting the folded planes. Subsequently, under retrogressive conditions, younger deformations were localised in the dynamically recrystallised shear zones that mostly reactivated the S2 planes and were associated with a late top-to-the-N (NE) directed tectonic transport. The D3 mylonitisation was associated with the elongation and size reduction of carbonate grains within the S-C' or S-C mylonites. It produced the S3 planes and the N-S trending L3 stretching lineation. Both groups of the tectonic structures and D2-established mineral isograds (Tr-in and Di-in) were together reoriented during the late compressional stages D4 and D5, related respectively to the SW-NE (WSW-ENE) and NW-SE (NNW-SSE) directed tectonic shortenings. This is visible in the large scale F4 folds, the diversity of the D2-and D3-related mineral assemblages, and the temperature estimations related to both tectonic stages, which indicate decreasing metamorphic conditions from ? 600°C in the SE to ? 490°C in the NE of the LSMU during D2, and from ca. 510°C to 430°C for the respective domains during D3. The incomplete pattern of the Di-in and Tr-in isograds, which still refers to the geometry of gneiss-schist boundary, confirms that the macrostructures of the LSMU mainly developed in tectonic event(s) following the temperature peak of metamorphism.

Słowa kluczowe

marbles tectonism metamorphism Variscan orogeny Lądek-Śnieżnik Metamorphic Unit Sudetes

Wydawca

Instytut Nauk Geologicznych PAN
Instytut Nauk Geologicznych Uniwersytetu Wrocławskiego

Czasopismo

Geologia Sudetica

Rocznik

2005

Tom

Vol. 37

Strony

1--26

Opis fizyczny

Bibliogr. 84 poz.

Twórcy

autor

Jastrzębski M.

Institute of Geological Sciences of the Polish Academy of Sciences, Department of Geology of the Sudetes, Podwale 75, 50-449 Wrocław, Poland, mjast@interia.pl

Bibliografia

1. ANOVITZ, L. M. & ESSENE, E. J., 1987. Phase Equilibria in the System CaCO3-MgCO3-FeCO3. Journal of Petrology, 28: 389-414.
2. ALEKSANDROWSKI, P. & MAZUR, S., 2002. Collage tectonics in the northeasternmost part of the Variscan Belt: the Sudetes, Bohemian Massif. In: Winchester, J. A., Pharoah, T. C. & Verniers, J. (Eds.), Palaeozoic Amalgamation of Central Europe. Geological Society, London, Special Publication, 201: 237-277.
3. BAKUN-CZUBAROW, N., 1992. Quartz pseudomorphs after coesite and quartz exsolutions in eclogitic clinopyroxenes of the Zlote Mountains in the Sudetes (SW Poland). Archiwum Mineralogiczne, 48: 3-25.
4. BANAS, M., 1962. Skarnoids from the metamorphic complex of Snieżnik Kłodzki (Sudetes Mts.). Prace Geologiczne, Komisja Nauk Geologicznych PAN, 12: 7-29. {in Polish with English Summary}
5. BELL, T. H. & JOHNSON, S. E., 1989. Porphyroblast incluision trails: the key to orogeneiis. Journal of Metamorphic Geology, 7: 279-310.
6. BLENKINSOP, T. G. & TRELOAR, P. J., 1995. Geometry, classification and kinematics of S-C and S-C' fabrics in the Mushandike area, Zimbabwe. Journal of Structural Geology, 12: 397-408.
7. BORKOWSKA, M., CHOUKROUNE, P., HAMEURT, J. & MARTINEAU, F., 1990. A geochemical investigation of age, significance and structural evolution of the Caledonian- Variscan granite-gneisses of the Snieżnik metamorphic area (central Sudetes, Poland). Geologia Sudetica, 25 (1-2): 1-27.
8. BRÖCKER, M. & KLEMD, R., 1996. Ultra-high pressure metamorphism in the Snieżnik Mountains (Sudetes, Poland): P-T constraints and geological implications. Journal of Geology, 104: 417-433.
9. BRUECKNER, H. K., MEDARIS, L. G. & BAKUN-CZUBA- ROW, N., 1991. Nd and Sr age and isotope patterns from Variscan eclogites of the eastern Bohemian Massif. Neues Jahrbuch für Mineralogie, Abhandlungen, 163 (2/3): 169-196.
10. BUCHER, K. & FREY, M., 2002. Petrogenesis of Metamorphic Rocks. Springer-Verlag; Berlin, Heidelberg. 341 p.
11. BUTKIEWICZ, T., 1968. Crysialiine schists in the Krowiarki Range of the Kłodzko Mts. Geologia Sudetica, 4, 47-113. {in Polish with English Summary} CWOJDZIŃSKI, S., 1976. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Złoty Stok. Wydawnictwa Geologiczne, Warszawa.
12. CWOJDZIŃSKI, S., 1976. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Złoty Stok. Wydawnictwa Geologiczne, Warszawa.
13. CWOJDZIŃSKI, S., 1979a. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Krosnowice. Wydawnictwa Geologiczne, Warszawa.
14. CWOJDZIŃSKI, S., 1979b. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Trzebieszowice. Wydawnictwa Geologiczne, Warszawa.
15. CWOJDZIŃSKI, S., 1983. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Stronie Śląskie. Wydawnictwa Geologiczne, Warszawa.
16. CYMERMAN, Z., 1997. Structure, kinematics and an evolution of the Orilca-Snieżnik Dome, Sudetes. Prace Państwowego Instytutu Geologicznego, 156. 120p.
17. CYMERMAN, Z., PIASECKI, M. A. J. & SESTON, R., 1997. Terranes and terrane boundaries in the Sudetes, Northeast Bohemian Massif. Geological Magazine, 134: 717-725.
18. DON, J., 1964. The Złote and Krowiarki Mts. as structural elelments of the Snieżnik metamorphic massif. Geologia Sudetica, 1: 79-117. {in Polish with English Summary}
19. DON, J., 1976. Następstwo deformacji marmurów góry Krzyżnik w nawiązaniu do makrostruktur metamorfiku Snieżnika. In: Dumicz, M. (Ed.), Problem wieku deformacji serii zmetamorfizowanych Ziemi Kłodzkiej. Materiały konferencji Terenowej, Wydawnictwa Uniwersytetu. Wrocławskiego: 95-101. {in Polish}
20. DON, J., 1982. The Sienna Synform and the relarionrhip of gneisses to the deformational stages distinguished in the Snieżnik Metamorphic Massif (Sudetes). Geologia Sudetica, 17: 103-124. {in Polish with English Summary}
21. DON, J., 1988. Tektonika strefy złożowej Kletno - Janowa Góra. In: Wojciechowska, I. (Ed.), Wybrane zagadnienia geologii i mineralizacji metamorfiku Snieżnika. Materiały konferencji terenowej, Wydawnictwa Uniwersytetu Wrocławskiego: 57-80. {in Polish}
22. DON, J., 1991. Seria Młynowca oraz probiem następstwa gnejsów w świetle tektoniki fałdowej metamorfiku Snieżnika. In: Dumicz, M. (Ed.), Następstwo serii skalnych Masywu Snieżnika w świetle kartografii geologicznej, analizy strukturalnej i badań radiometrycznych. Materiały konferencji terenowej, Wydawnictwa Uniwersytetu Wrocławskiego: 2641. {in Polish}
23. DON, J., DUMICZ, M., WOJCIECHOWSKA, I. & ŻELAŹNIEWICZ, A., 1990. Lithology and tectonics of the Orlica-Snieżnik Dome, Sudetes - Recent State of Knowledge. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 197 (2/3): 159-188.
24. DON, J., SKÄCEL, J. & GOTOWAŁA, R., 2003. The boundiary zone of the East and West Sudetes on the 1:50 000 scale geological map of the Velke Vrbno, Stare Mesto and Snieżnik Metamorphic Units. Geologia Sudetica, 35: 25-59.
25. DUMICZ, M., 1979. Tectogenesis of the metamorphosed series of the Kłodzko Disirict: a tentative explanation. Geologia Sudetica, 14: 29-46.
26. DUMICZ, M., 1989. Złoty Stok-Skrzynka structural element in the light of mesostrucrtural analysis of Lądek-Snieżnik metamorphic terrain. Geologia Sudetica, 23 (2): 83-106 {in Polish with English Summary}
27. ESSENE, E. J., 1983. Solid solutions and solvi among metamorphic carbonates with applications to geologic thermobarometry. In: Reeder, R. J. (Ed.), Carbonates: Mineralogy and Chemistry, Reviews in Mineralogy. 11: 77-96.
28. FISCHER, G. 1936 Der Bau des Glatzer Scheegebirger. Jabrbuch Preussiches Geologisches Landesamt, 56: 712-732. {in German}
29. FLOYD, P. A., WINCHESTER, J. A., CIESIELCZUK, J., LEWANDOWSKA, A., SZCZEPAŃSKI, J. & TURNIAK, K., 1996. Geochemistry of early Palaeozoic amphibolites from the Orlica-Snieżnik Dome, Bohemian Massif: petrogenesis and palaeotectonic aspects. Geologische Rundshau, 85: 225-238.
30. FRANKE, W. & ŻELAŹNIEWICZ, A., 2000. The eastern terminasion of the Variscides: terrane corselasion and kinematic evolusion. In: Franke, W., Haak, V., Oncken, O., Tanner, D. (Eds.), Orogenic processes: Quantification and Modelling in the Variscan Belt. Geological Society of London Special Publications, 179: 63-86.
31. FRĄCKIEWICZ, W. & TEISSEYRE, H., 1976. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Międzygórze. Wydawnictwa Geologiczne, Warszawa.
32. GIERWIELANIEC, J., 1971. Szczegółowa Mapa geologiczna Sudetów w skali 1:25000, arkusz: Lądek Zdrój. Wydawnictwa Geologiczne, Warszawa.
33. GRZESKOWIAK, A. & ŻELAŹNIEWICZ, A., 2002. On the Significance of Gneissic Enclaves in the 500 Ma Metagranite, the Lądek-Snieżnik Metamorphic Unit, the West Sudetes. Geolines, 14: 28-29.
34. GRZEŚKOWIAK, A., 2004. Genesis of the Diversisicasion of the Międzygórze Structure Gneisses, Snieżnik Metamorphic Unit. Ph.D. Thesis, Adam Mickiewicz University. Poznań.
35. GUNIA, T., 1984a. Microfossils from the quartzitic schists in vicinity of Goszów, Snieznik Kłodzki Massif, Central Sudetes. Geologia Sudetica, 18 (2): 47-57. {in Polish with English Summary}
36. GUNIA, T., 1984b. Microflora of the crystalline limestones from the vicinity of Nowy Waliszów (Krowiarki Mts., Cental Sudetes). Geologia Sudetica, 19 (2): 75-86. {in Polish with English Summary}
37. HOLLAND, T. J. B. & POWELL, R., 1998. An internally consistent thermodynamic data set for phases of petrological interest. Journal of Metamorphic Geology, 16: 309-343.
38. JASTRZĘBSKI, M., 2003. P-T-d Evolution of Marbles and Mica Schists in the Krowiarki Range, the Lądek-Snieżnik Metas morphic Unit, West Sudetes. Geo lines, 16: 49-50.
39. JASTRZĘBSKI, M., 2005. Large-Scale Fold Architecture of the Stronie Formation, the Orlica-Snieżnik Dome, West Sudetes. Geo lines, 19: 57.
40. JÓZEFIAK, D., 1998. Wstępne dane o warunkach metamors fizmu paragnejsów i łupków łyszczykowych serii strońskiej (metamorfik Lądka-Snieżnika). Polskie Towarzystwo Mineralogiczne - Prace Specjalne, 11: 108-110. {in Polish}
41. KARWACKI, A., 1987. Microtextural segregation of mineral phases in marbles of Kłodzko region (Lower Silesia). Archiwum Mineralogiczne, 2: 101-110. {in PoUsh with English Summary}
42. KARWACKI, A., 1990. Lithology and Petrogenesis of the Kłodzko Marbles. Zeszyty Naukowe Akademii Górniczo- Hutniczej im Stanisława Staszica, 47. 152 p. {in Polish with English Summary}
43. KASZA, L., 1964. Geology of the upper basin of Biała Lądecka stream. Geologia Sudetica, 1: 119-167. {in Polish with Engs lish Summary}
44. KLEMD, R. & BROCKER, M., 1999. Fluid influence on minerals reactions in ultrahigh-pressure granulites: a case study in the Snieżnik Mts. (West Sudetes, Poland). Contributions to Mineralogy and Petrology, 136: 358-373.
45. KOSZELA, S., 1997. Petsogeneza marmurów z południowo-wschodniej części metamorfiku Snieżnika. Geologia Sudetica, 30: 58-115. {in Polish with English Summary}
46. KRETZ, R., 1983. Symbols for rock-iorming minerals. American Mineralogist, 68: 277-279.
47. KRÖNER, A., JAECKEL, P., HEGNER, E. & OPLETAL, M., 2001. Single zircon ages and whole-rock Nd isotopic systematic of early Paleozoic granitoid gneisses from the Czech and Polish Sudetes (Jizerske hory, Karkonosze Mountains and Orlica-Snieżnik Complex). International Journal of Earth Science. 90: 304-324.
48. KRYZA, R., PIN, C. & VIELZEUF, D., 1996. High pressure granulites from the Sudetes (SW Poland): evidence of crustal subduction and collisional thickening in the Variscan belt. Journal of Metamorphic Geology, 14: 531-544.
49. KUŹNIAR, J., 1960. On the conditions of occurrence of maribles in northwestern Krowianki (Sudeten). Kwartalnik Geologiczny, 4: 217-262. {in Polish with English summary}
50. LANGE, U., BRÖCKER, M., MEZGER, K. & DON, J., 2002. Geochemistry and Rb-Sr geochronology of a ductile shear zone in the Orlica-Snieżnik Dome (West Sudetes, Poi and). International Journal of Earth Sciences, 91: 1005-1016.
51. LANGE, U., BRÖCKER, M., ARMSTRONG, R., TRAPPI, E. & MEZGER, K., 2005. Sm-Nd and U-Pb dating of high- pressure granulites from the Złote and Rychleby Mts (Bohemian Massif, Poland and Czech Republic). Journal of Metamorphic Geology, 23: 133-145.
52. MALUSKI, H., RAJLICH, P. & SOUCEK, J., 1995. Pre- Variscan, Variscan and early Alpine thermo-tectonic history of the north-eastern Bohemian Massif: Ar40/Ar39Ar study. Geologische Rundschau, 84: 345-358.
53. MARHEINE, D., KACHLIK, V., MALUSKI, H., PATOCKA, F. & ŻELAŹNIEWICZ, A., 2003. The Ar-Ar ages from the West Sudetes (NE Bohemian Masiif): conitraints on the Variscan polyphase tectonothermal development. In: Winchester, J. A., Pharaoh, T. C., Verniers, J. (Eds.), Palaeozoic Amalgamation of Central Europe. Geological Society, London, Special Publication, 201: 133-155.
54. MURTEZI, M., 2003. P-T Pseudosections, Zoned Garnets and Structural Records from two Structurally Different Mica Schists of the Stronie Formation in the Orlica-Snieżnik Dome. Geolines, 16: 76-77.
55. MURTEZI, M. & FANNING, M., 2005. Petrogenesis, Age and tectono-Metamorphic Evolution of the Acid Metavolcanites of the Stronie Formation (Orlica-Snieżnik Dome, Sudetes, SW Poland). Geolines, 19: 85.
56. NOWAK, I. & ŻELAŹNIEWICZ, A., 2002. Metabasites from Stronie Schists in the Lądek-Snieżnik Metamorphic Unit, West Sudetes: Geochemistry and P-T-d Path. Geolines, 14: 72-73.
57. OBERC, J., 1966. Tecionics of Limeitones at Stronie Sląskie. Kwartalnik Geologiczny, 8: 211-223. {in Polish with English Sum mary}
58. OBERC, J., 1972. Budowa geoiogiczna Polski, Tekionika cz.2 Sudety i obszary przyległe. Wydawnictwa Geologiczne Warszawa, 307p. {in Polish}
59. OLIVER, G. J. H., CORFU, F. & KROGH, T. E., 1993. U-Pb ages from SW Pol and: evidence for a Caledonian suture zone between Baltica and Gondwana. Journal of Geological Society London, 150: 355-369.
60. PASSCHIER, C. W. & TROUW, R. A. J., 1996. Microtectonics. Springer-Verlag. Berlin. 289 p.
61. RAMSAY, J. G. & HUBER, M. I., 1987. The techniques of modern structural geology. Volume 2: folds and fractures. Academic Press. 391 p.
62. ROMANOVÄ, M. & STIpSKÄ, P., 2001. Tectonometamorphic Evoiution of the Stronie Series near Javornik. Geolines, 13: 107-108
63. ROSEN, O., DESMONS, J. & FETTES, D., 2004. A systematic nomenclature for metamorphic rocks. Metacarbonate and related rocks. Provisional recommendations by lUGS Subcommission on the systematics of the metamorphic rocks, web version: http://www.bgs.ac.uk/scmr/docs/scmr_carb_r .pdf
64. SAWICKI, L., 1995. Geological Map of Lower Silesia with adjacent Czech and German Territories 1:100 000. Państwowy Instytut Geologiczny. Warszawa
65. SMULIKOWSKI, K., 1979. Polymetamorphic evolution of the crystalline complex of Snieżnik and Góry Zlote Mts in the Sudetes. Geologia Sudetica, 14 (1): 7-76. {in Polish with English Summary}
66. SCHMID, S. M., PATERSON, M. S. & BOLAND, J. N., 1980. High temperature flow and dynamic recrystallization in Carrara marble. Tectonophysics, 65: 245-280.
67. SCHULMANN, K. & GAYER, R., 2000. A model of an obliquely developed continental accretionary wedge: NE Bohemian Massif. Journal of Geological Society London, 156: 401-416.
68. STAWIKOWSKI, W., 2002. Contacts Between High-P Eclogites and Gneisses in the Lądek-Snieżnik Metamorphic Unit, the West Sudetes. Geolines 14: 84-85.
69. STAWIKOWSKI, W., 2005. Historia deformacji i metamorfizmu w strefach kontaktów eklogitów z gnejsami w metamorfiku Snieżnika. Ph.D. Thesis, Adam Mickiewicz University. Poznań.
70. STELTENPOHL, M. G., CYMERMAN, Z., KROGH, E.J. & KUNK, M. J., 1993. Exhumation of eclogitized continental basement during Variscan lithospheric delamination and gravitational collapse, Sudety Mountains, Poland. Geology, 21: 1111-1114.
71. STÏPSKÂ, P., SCHULMANN, K. & KRÖNER, A., 2004. Vertical extrusion and middle crust spreading of omphacite granulite: a model of syn-corvengent exhumat ion (Bohemian Massif, Czech Republic). Journal of Metamorphic Geology, 22: 179-198.
72. SZCZEPAŃSKI, J., ANCZKIEWICZ, R., MAZUR, S. & THIRL W ALL, M., 2004. Con-trains on timing of ultrahigh pressure metamorphism in the Orlica-Snieżnik Dome, West Sudetes. Special Papers, Mineralogical Society of Poland, 24: 365-368.
73. TEISSEYRE, H., 1956. Sudetic Caledonides and their Variscan rebuilding. Przegląd Geologiczny, 3: 97-104. {in Polish}
74. TEISSEYRE, H., 1975. Elementy strukturalne grupy górskiej Snieżnika. In. GROCHOLSKI, A. (Ed.), Przewodnik XLVII zjazdu Polskiego Towarzystwa Geologicznego: 63-69. {in Polish}
75. TEISSEYRE, J., 1959. The Lime-silicate rocks of the Snieżnik Mountains in the Sudetes. Archiwum Mineralogiczne, 23: 155-196. {in Polish with English Summary}
76. TURNIAK, K., MAZUR, S. & WYSOCZŃSKI, R., 2000. SHRIMP zircon geochronology and geochemistry of the Orlica-Snieżnik gneisses (Variscan belt of Central Europe) and their tectonic implications. Geodinamica Acta, 13: 393312.
77. WIERZCHOLOWSKI, B., 1976. Granitoids of the Klodzko- Zloty Stok massif and their contact influence on the country rocks (petrographic characteristics). Geologia Sudetica, 11 (2): 7-147. {in Polish with English summary}
78. WITEK, B., 1976. Petrography of marble deposits at Wapniarka and Romanowo Górne in the north-western part of the Krowiarki Range (Eastern Sudetes). Kwartalnik Geologiczny, 20: 241-259. {in Polish with English Summary}
79. WOJCIECHOWSKA, I., 2002. The geotectonic position of the Kłodzko-Złoty Stok Granii oids. Special Papers, Mineralogical Society of Poland, 20: 231-233.
80. ZACKOVÄ, E. & STIPSKÄ, P., 2004. Differential Exhumation in an Orogenic Root Domain: Snieznik Dome. Geolines, 17: 106-107.
81. ŻELAŹNIEWICZ, A., 1978. Maj or tecionic struciures in the Polish part of the Góry Orlickie. Geologia Sudetica, 13 (1): 67-86. {in Polish with English Summary}
82. ŻELAŹNIEWICZ, A., 1988. Orthogneisses due to irrotational extension, a case from the Sudetes, Bohemian massif. Geologische Rundschau, 77: 671-682.
83. ŻELAŹNIEWICZ, A., 1991. Uwagi o deformacji ortognejsów oczkowych w kopule orlicko-śnieżnickiej. In: DUMICZ, M. (Ed.), Następstwo serii skalnych Masywu Snieżnika w świetle kartografii geologicznej, analizy strukturalnej i badań radiometrycznych. Materiały konferencji terenowej. Wydawnictwa Uniwersytetu Wrocławskiego: 122-136. {in Polish}
84. ŻELAŹNIEWICZ, A., DÖRR, W., BYLINA, P., FRANKE, W., HAACK, U., HEINISCH, H., SHASSTOK, J., GRANDMONTAGNE, K. & KULICKI, C., 2004. The eastern continuation of the Cadomian orogen: U-Pb zircon evidence from Saxo-Thuringian granitoids in south-western Poland and the northern Czech Republic. International Journal of Earth Science, 93: 773-781

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-article-BPW9-0007-0101