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Synsedimentary seismotectonic features in Triassic and Cretaceous sediments of the Intrasudetic Basin (U Devěti křížů locality) – regional implication

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EN
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EN
Synsedimentary deformation structures have been recognized in Triassic and Cretaceous sedimentary rocks of the Trutnov Basin, which build a structural and morphological elevation between Červený Kostelec and Upice. Very well preserved sand injection and collapse structures, strike-slip shearings and listric faults occur in the “U Devěti křížů” Quarry. Their shapes and spatial distribution strongly correspond to local tectonic structures within the Intrasudetic Shear Zone (ISZ), especially to the faults which bound the rhomb-shaped depressions and elevations. All these structural sub-units compose the Intrasudetic Basin Suite (IBS). The soft-sediment deformations developed in the shallow subsurface and most likely resulted from the dominantly extensional and strike-slip kinematics within the ISZ.
Słowa kluczowe
Rocznik
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355--364
Opis fizyczny
Bibliogr. 65 poz., rys.
Twórcy
autor
  • Wrocław University, Institute of Geological Sciences, Pl. M. Borna 9, 50-204 Wrocław, Poland
autor
  • Wrocław University, Institute of Geological Sciences, Pl. M. Borna 9, 50-204 Wrocław, Poland
autor
  • Wrocław University, Institute of Geological Sciences, Pl. M. Borna 9, 50-204 Wrocław, Poland
Bibliografia
  • 1. Audemard, F.A., Gómez, J.C., Taverab, H.J., Orihuela, N., 2005. Soil liquefaction during the Arequipa Mw 8.4, June 23, 2001 earthquake, southern coastal Peru. Engineering Geology, 78: 237-255.
  • 2. Berg, G., 1909. Erläuterungen zur Geologischen Karte von Preußen und benachbarten Bundesstaaten. Liefferung 145, Blatt Schömberg. Preußischen Geologischen Landesanstalt, Berlin.
  • 3. Beyrich, F., 1854. Über die Lagerung der Kreideformation im Schlesien. Abhandlungen Preußen Akademie der Wissenschaften, 26: 57-80.
  • 4. Bonini, M., 2009. Mud volcano eruptions and earthquakes in the Northern Apennines and Sicily, Italy. Tectonophysics, 474: 723-735.
  • 5. Bonini, M., Sani, F., 2000. Thrusting, strike-slip faulting and syntectonic deposition in the Potenza-Guardia Perticara Area (Basilicata, Southern Apennines, Italy). Memorie della Societa Geologica Italiana, 55: 123-132.
  • 6. Bureau, D., Mourgues, R., Cartwright, J., 2014. Use of a new artificial cohesive material for physical modelling: application to sandstone intrusions and associated fracture networks. Journal of Structural Geology, 66: 223-236.
  • 7. Burliga, S., Martinek, K., Wojewoda, J., 2008. Perm karkonoskiego basenu piedmontowego i basenu Nachodu (in Polish). In: Baseny śródgórskie: kontekst regionalny środowisk i procesów sedymentacji (ed. J. Wojewoda): 64-110. Materiały Konferencyjne, wycieczka C WIND, Kudowa Zdrój, 15-21.09.2008.
  • 8. Carter, R.M., Norris, R.J., 1986. Redeposited conglomerates in a Miocene flysch sequence at Blackmount, Western Southl and, New Zealand. Sedimentary Geology, 18: 289-319.
  • 9. Childs, C., Nicol, A., Watterson, J., Walsh, J.J., 1996. Fault overlap zones within developing normal fault systems. Journal of Structural Geology, 18: 1389-1397.
  • 10. Dathe, E., Zimmermann, E., Berg, G., 1910. Erläuterungen zur Geologischen Karte von Preußen und benachbarten Bundesstaaten. Liefferung 145, Blatt Friedland. Preußischen Geologischen Landesanstalt, Berlin: 1-64.
  • 11. Don, J., Jerzykiewicz, T., Teisseyre, A.K., Wojciechowska, I., 1981. Szczegółowa Mapa Geologiczna Sudetów 1:25 000, arkusz Lubawka (in Polish). Instytut Geologiczny, Warszawa.
  • 12. Dornbos, S.Q., Noffke, N., Hagadorn, J.W., 2007. Mat-decay features. In: Atlas of Microbial Mat Features Preserved within the Clastic Rock Record (eds. J. Schieber, P.K. Bose, P.G. Eriiksson, S. Banerjee, S. Sarkar, W. Altermann and O. Catuneau): 106-110. Elsevier, Amsterdam.
  • 13. Dunne, W.M., Hancock, P.L., 1994. Palaeostress Analysis of Small-Scale Brittle Structures. Chapter 5. In: Continental Deformation (ed. P.L. Hancock): 101-120. Pergamon Press.
  • 14. Flegel, K., 1905. Heuscheuer und Adersbach-Weckelsdorf. Eine Studie über die obere Kreide im böhmisch-schlesischen Gebirge (Dissertation): 1-36.
  • 15. Grocholski, A., 1973. Szczegółowa Mapa Geologiczna Sudetów 1:25 000, arkusz Mieroszów (in Polish). Instytut Geologiczny, Warszawa.
  • 16. Hancock, P.L., 1985. Brittle microstrutures: principles and practice. Journal of Structural Geology, 7: 437-457.
  • 17. Hancock, P.L., Al Kadhi, A., Barka, A.A., Bevan, T.G., 1987. Aspects of analysing brittle structures. Annales Tectonicae, 1: 5-19.
  • 18. Hilbert-Wolf, H.L., Simpson, E.L., Simpson, W.S., Tindall, S.E., Wizevich, M.C., 2009. Insights into syndepositional fault movement in a foreland basin; trends in seismites of the Upper Cretaceous, Wahweap Formation, Kaiparowits Basin, Utah, USA. Basin Research, 21: 856-871.
  • 19. Holub, V., 1966. Geologické Poměry Východního Podkrkonoší. Unpublished report (in Czech). Geofond ČR, Prague.
  • 20. Holub, V., 1972. Permian of the Bohemian Massif. In: Rotliegend Essays on European Lower Permian (ed. H. Falke): 137-188. E. J. Brill (Holland).
  • 21. Holub, V., Tásler, R., 1974. Mladší paleozoikum a spodní trias v podloží ceské křídové pánve (in Czech). In: Geologie ceské křídové pánve a jejího podloží (ed. M. Malkovský): 72-100. Ústřední Ústav Geologický, Praha.
  • 22. Hurst, A., Scott, A., Vigorito, M., 2011. Physical characteristics of sand injectites. Earth-Science Reviews, 106: 215-246.
  • 23. Jerzykiewicz, T., 1971. Cretaceous in the vicinity of Krzeszów (in Polish with English summary). Geologia Sudetica, 5: 281-327.
  • 24. Kattenhorn, S.A., Aydin, A., Pollard, D.D., 2000. Joints at high angles to normal fault strike: an explanation using 3-D numerical models of fault-perturbed stress fields. Journal of Structural Geology, 22: 1-23.
  • 25. Maltman, A., 1994. The Geological Deformation of Sediments. Chapman and Hall.
  • 26. Martin-Chivelet, J., Palma, R.M., Lopez-Gomez, J., Kietzmann, D.A., 2011. Earthquake-induced soft-sediment deformation structures in Upper Jurassic open-marine microbialites (Neui quen Basin, Argentina). Sedimentary Geology, 235: 210-221.
  • 27. Mazumder, R., Rodríguez-López, J.P., Arima, M., Van Loon, A.J., 2009. Palaeoproterozoic seismites (fine-grained facies of the Chaibasa Fm., E India) and their soft-sediment deformation structures. Geological Society Special Publications, 323: 301-318.
  • 28. Mikuláš, R., Prouza, V., 1999. The Cretaceous biogenic structures created in Triassic sandstones (Devět křížů at Červený Kostelec, NE Bohemia, Czech Republic). Věstník Českého Geologického Ústavu, 74: 335-342.
  • 29. Mikuláš, R., Plièka, M., Skalický, J., 1991. A find of mud scrolls in Lower Triassic sandstone at the locali ty Devět křížů (NE Bohemia). Věstník Českého Geologického Ústavu, 66: 247-249.
  • 30. Moretti, M., Sabato, L., 2007. Recognition of trigger mechanisms for soft-sediment deformation in the Pleistocene lacustrine deposits of the Sant’Arcangelo Basin (Southern Italy): seismic shock vs. overloading. Sedimentary Geology, 196: 31-45.
  • 31. Moretti, M., Alfaro, P., Caselles, O., Canas, J.A., 1999. Modelling seismites with a digital shaking table. Tectonophysics, 304: 369-383.
  • 32. Mroczkowski, J., Mader, D., 1985. Sandy inland braidplain deposition with local aeolian sedimentation in the lower and middle parts of the Buntsandstein and sandy coastal braidplain deposition in the topmost Zechstein in the Sudetes (Lower Silesia, Poland). Lecture Notes in Earth Sciences, 4: 165-195.
  • 33. Müller, G., 1930. Der kontinentale Zechstein im Süden des Riesengebirges. Abhandlungen der Preußischen Geologischen Landesanstalt, N.F., Berlin, 130: 1-90.
  • 34. Neuwerth, R., Suter, F., Guzman, C.A., Gorin, G.E., 2006. Soft-sediment deformation in a tectonically active area: the Plio-Pleistocene Zarzal Formation in the Cauca Valley (Western Colombia). Sedimentary Geology, 198: 67-88.
  • 35. Petrascheck, W., 1933. Der böhmische Anteil der Mittelsudeten und sein Vorland. Mitteilungen der Geologischen Gesellschaft in Wien, 26: 1-136.
  • 36. Pollard, D.D., Aydin, A., 1988. Progress in understanding jointing over the past century. GSA Bulletin, 100: 1181-1204.
  • 37. Porada, H., Bouougri, E., 2007. “Wrinkle structures” - a critical review. In: Atlas of Microbial Mat Features Preserved within the Clastic Rock Record (eds. J. Schieber, P.K. Bose, P.G. Erii ksson, S. Banerjee, S. Sarkar, W. Altermann and O. Catuneau): 135-144. Elsevier, Amsterdam.
  • 38. Prave, A.R., 2002. Life on land in the Proterozoic: evidence from the Torridonian rocks of northwest Scotland. Geology, 30: 811-814.
  • 39. Prouza, V., 1988. Geologická Mapa ČSR (in Czech). List 04-32 Broumov, 1:50 000. Ústřední Ústav Geologický, Praha.
  • 40. Prouza, V., Tásler, R., 1985. Přehledná geologická mapa podkrkonošské pánve (in Czech). Ústřední Ústav Geologický, Praha.
  • 41. Prouza, V., Tásler, R., Valín, F., Holub, V., 1985. Gravelly to sandy braidplain deposition in the Buntsandstein-facies Bohdašín Formation in Northeastern Bohemia (Czechoslovakia). Lecture Notes in Earth Sciences, 4: 397-410.
  • 42. Rodrigues, N., Cobbold, P.R., Lrseth, H., 2009. Physical modelling of sand injectites. Tectonophysics, 474: 610-632.
  • 43. Stewart, S.A., Hancock, P., 1991. Scales of structural heterogeneity with neotectonic normal fault zones in the Aegean region. Journal of Structural Geology, 13: 191-204.
  • 44. Taj, R.J., Aref, M.A.M., Schreiber, B.C., 2014. The influence of microbial mats on the formation of sand volcanoes and mounds in the Red Sea coastal plain, south Jeddah, Saudi Arabia. Sedimentary Geology, 311: 60-74.
  • 45. Tásler, R., 1961. Prehled geologie permokarbonu a spodniho triasu (in Czech). In: Vysvetlivky k prehledne geolicke mape CSSR (eds. J. Svoboda and J. Chaloupsky). Ústřední Ústav Geologický, Praha.
  • 46. Tásler, R., 1966. Triassic. In: Regional Geology of Czechoslovakia, part I: the Bohemian Massif (eds. J. Svoboda et al.): 481-483. Publishing House of the Czechoslovakia Academy of Sciences, Prague.
  • 47. Ulièný, D., 2004. A dryi ng-upward aeolian system of the Bohdašín Formation (Early Triassic), Sudetes of NE Czech Republc: record of seasonali ty and long-term palaeoclimate change. Sedimentary Geology, 167: 17-39.
  • 48. Ulièný, D., Špičáková, L., Grygar, R., Svobodová, M., Èech, S., Laurin, J., 2009. Palaeodrainage sysiems at the basal unconformity of the Bohemian Cretaceous Basin: roles of inherited fault systems and basement lithology duri ng the onset of basin filling. Bulletin of Geosciences, 84: 577-610.
  • 49. Valín, F., 1964. Litologie triasu v severovýchodních Čechách (in Czech). Věstník Českého Geologického Ústavu, 39: 459-462.
  • 50. Van Loon, A.J., Maulik, P., 2011. Abraded sand volcanoes as a tool for recognizing paleo-earthquakes, with examples from the Cisuralian Talchir Formation near Angul (Orissa, eastern India). Sedimentary Geology, 238: 145-155.
  • 51. Vanneste, K., Meghraoui, M., Camelbeeck, T., 1999. Late Quaternary earthquake-related soft-sediment deformation along the Belgian portion of the Feldbiss Fault, Lower Rhine Graben system. Tectonophysics, 309: 57-79.
  • 52. Vejlupek, M., 1983. Ke stratigrafické pozici devítikřížských pískovců (in Czech). Véstník Českého Geologického Ústavu, 58: 57-59.
  • 53. Walsh, J.J., Bailey, W.R., Childs, C., Nicol, A., Bonson, C.G., 2003. Formation of segmented normal faults: 3-D perspective. Journal of Structural Geology, 25: 1251-1262.
  • 54. Wang, X., 1995. Estimation of the variation in apparent displacement along normal fault traces refracted by differential compaction. Journal of Structural Geology, 17: 191-204.
  • 55. 57. Wojewoda, J., 2007a. Palaeogeography and tectonic evolution of the Žernov-Nachod-Kudowa sedi mentary area. In: 5th Meeting of the Ceniral European Tectonic Studies Group (CETEG'5), April 11-14.04.2007, Tepla.
  • 56. Wojewoda, J., 2007b. Žďárky-Pst^žna Dome - dextral strike-slip fault-related structure at the eastern termination of the Poriči-Hronov Fault Zone (Sudetes, Góry Stołowe Mts.). In: 5th Meeting of the Central European Tectonic Studies Group (CETEG'5), April 11-14.04.2007, Tepla.
  • 57. Wojewoda, J., 2007c. Neotectonic aspect of the Intrasudetic Shear Zone. Acta Geodynamica et Geomaterialia, 4: 1-11.
  • 58. Wojewoda, J., 2007d. Perm basenu Nachodu. Sedimentologica, 1: 85-99.
  • 59. Wojewoda, J., 2008a. Post-Variscan evolution of the Poříčí-Hronov zone. 9th Czech-Polish Workshop on Recent Geodynamics of the Sudeten and Adjacent Areas, 12-15.11.2008, Náchod, Astracts: 27-28.
  • 60. Wojewoda, J., 2008b. Poříčí-Hronov strike-slip zone related structures. 9th Czech-Polish Workshop on Recent Geodynamics of the Sudeten and Adjacent Areas, 12-15.11.2008, Náchod, Astracts: 29-30.
  • 61. Wojewoda, J., 2009a. Žďarky-Pst^žna Dome: a strike-slip fault-related structure at the eastern termination of the Poříčí-Hronov Fault Zone (Sudetes). Acta Geodynamica et Geomaterialia, 6: 273-290.
  • 62. Wojewoda, J., 2009b. The role of the Poříčí-Hronov Fault Zone in foundation of sudetic basins. In: 7th Meeting of the Central European Tectonic Studies Group (CETEG'7), 13-16.05.2009, Pecs. Abstracts.
  • 63. Wojewoda, J., 2009c. Poříčí-Hronov Fault Zone: Malé Svatoňovice. 10th Czech-Poli sh Workshop on Recent Geodynamics of the Sudeten and Adjacent Areas, 5-7.11.2009, Szklarska Poręba, Poland.
  • 64. Wojewoda, J., Mastalerz, K., 1989. Climate evolution and alloand autocyclic sedimentation of Upper Carboniferous and Permian contiental deposits in the Sudetes (in Polish with English summary). Przegląd Geologiczny, 37: 173-180.
  • 65. Zajíc, J., 1998. The first find of the dinosaurian footprint in the Czech Republic (the Krkonoše Piedmont Basin) and its stratigraphic significance. Journal of the Czech Geological Society, 43:273-275.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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