Deciphering the Variscan tectonothermal overprint and deformation partitioning in the Cadomian basement of the Teplá-Barrandian unit, Bohemian Massif

International Journal of Earth Sciences

Volumn 101, Issue 7, 2012, Pages 1855-1873

  Hajná, Jaroslava ^a   Žák, Jiří ^a   Kachlík, Václav ^a   Chadima, Martin ^b,c  

^a CHARLES UNIVERSITY   (Czech Republic)

^b Advanced Geoscience Instruments Company   (Czech Republic)

^c INSTITUTE OF GEOLOGY   (Czech Republic)

Author keywords

Avalonian Cadomian belt; Bohemian Massif; Shear zone; Tepl Barrandian unit; Transpression; Variscan orogeny

Indexed keywords

AVALONIA; BASEMENT ROCK; CADOMIAN OROGENY; DEFORMATION; GONDWANA; HERCYNIAN OROGENY; MAGNETIC SUSCEPTIBILITY; OROGENIC BELT; OROGENY; OVERPRINTING; PARTITIONING; PROTEROZOIC; SHEAR ZONE; SUBDUCTION ZONE; TRANSPRESSION; UPPER CRUST;

BOHEMIAN MASSIF; CZECH REPUBLIC; TEPLA-BARRANDIAN;

EID: 84866469090     PISSN: 14373254     EISSN: 14373262     Source Type: Journal    
DOI: 10.1007/s00531-012-0753-8     Document Type: Article

References (98)

1. Babuška V, Fiala J, Plomerová J (2010) Bottom to top lithosphere structure and evolution of western Eger Rift (Central Europe). Int J Earth Sci 99:891-907
2. Badham JP (1982) Strike slip orogens-an explanation for the Hercynides. J Geol Soc London 139:495-506
3. Borradaile GJ, Jackson M (2010) Structural geology, petrofabrics and magnetic fabrics (AMS, AARM, AIRM). J Struct Geol 32:1519-1591
4. Burg JP (1999) Ductile structures and instabilities: their implication for Variscan tectonics in the Ardennes. Tectonophysics 309:1-25
5. Čech S, Havlíček V, Zikmundová J (1988) Upper Devonian and Lower Carboniferous in north-eastern Bohemia (based on boreholes in the Hradec Králové area). Bull Central Geol Surv 64:65-75
6. Cháb J, Žáček V (1994) Metamorphism of the Teplá Crystalline complex. KTB Rep 94:33-37
7. Cháb J, Suchý V, Vejnar Z (1995) Teplá-Barrandian Zone (Bohemicum): metamorphic evolution. In: Dallmeyer RD, Franke W, Weber K (eds) Pre-Permian geology of central and eastern Europe. Springer, Berlin, pp 404-410
8. Chlupá ČI, Zikmundová J (1976) The Devonian and lower Carboniferous in the Nepasice bore in east Bohemia. Bull Central Geol Surv 51:269-278
9. Chlupáčová M, Hrouda F, Janák J, Rejl L (1975) The fabric, genesis and relative age relations of the granitic rocks of the Čistá-Jesenice massif. Gerlands Beitr Geophys 84:487-500
10. Crowley QG, Floyd PA, Winchester JA, Franke W, Holland JG (2000) Early Palaeozoic rift-related magmatism in Variscan Europe: fragmentation of the Armorican Terrane Assemblage. Terra Nova 12:171-180
11. Crowley QG, Timmermann H, Noble SR, Holland JG (2002) Palaeozoic terrane amalgamation in central Europe: a REE and Sm-Nd isotope study of the pre-Variscan basement, NE Bohemian Massif. In: Winchester JA, Pharaoh TC, Verniers J (eds) Palaeozoic amalgamation of central Europe. Geol Soc London Spec Publ 201:157-176
12. Dallmeyer RD, Urban M (1994) Variscan vs. Cadomian tectonothermal evolution within the Teplá-Barrandian zone, Bohemian Massif, Czech Republic: evidence from 40Ar/39Ar mineral and whole-rock slate/phyllite ages. J Czech Geol Soc 39:21-22
13. 39Ar ages. Geol Rundsch 87:94-106
14. Dörr W, Zulauf G (2010) Elevator tectonics and orogenic collapse of a Tibetan-style plateau in the European Variscides: the role of the Bohemian shear zone. Int J Earth Sci 99:299-325
15. Dörr W, Fiala J, Vejnar Z, Zulauf G (1998) U-Pb zircon ages and structural development of metagranitoids of the Teplá crystalline complex-evidence for pervasive Cambrian plutonism within the Bohemian Massif (Czech Republic). Geol Rundsch 87:135-149
16. Dörr W, Zulauf G, Fiala J, Franke W, Vejnar Z (2002) Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá-Barrandian unit-a correlation of U-Pb isotopicdilution TIMS ages (Bohemia, Czech Republic). Tectonophysics 352:65-85
17. Dostal J, Patočka F, Pin C (2001) Middle/Late Cambrian intracontinental rifting in the central west Sudetes, NE Bohemian Massif (Czech Republic): geochemistry and petrogenesis of the bimodal metavolcanic rocks. Geol J 36:1-17
18. Drost K, Linnemann U, McNaughton N, Fatka O, Kraft P, Gehmlich M, Tonk C, Marek J (2004) New data on the Neoproterozoic- Cambrian geotectonic setting of the Teplá-Barrandian volcanosedimentary successions: geochemistry, U-Pb zircon ages, and provenance (Bohemian Massif, Czech Republic). Int J Earth Sci 93:742-757
19. Drost K, Gerdes A, Jeffries T, Linnemann U, Storey C (2011) Provenance of Neoproterozoic and early Paleozoic siliciclastic rocks of the Teplá-Barrandian unit (Bohemian Massif): evidence from U-Pb detrital zircon ages. Gondwana Res 19:213-231
20. Dubanský A (1984) Determination of the radiogenic age by the K-Ar method (geochronological data from the Bohemian Massif in the ČSR region). Collect Sci Works Tech Univ Ostrava 30:137-170
21. Filip J, Suchý V (2004) Thermal and tectonic history of the Barrandian Lower Paleozoic, Czech Republic: is there a fission-track evidence for Carboniferous-Permian overburden and pre-Westphalian alpinotype thrusting? Bull Geosci 79:107-112
22. Floyd PA, Winchester JA, Seston R, Kryza R, Crowley QG (2000) Review of geochemical variation in Lower Palaeozoic metabasites from the NE Bohemian Massif: intracratonic rifting and plume-ridge interaction. In: Franke W, Haak V, Oncken O, Tanner D (eds) Orogenic processes: quantification and modelling in the Variscan belt. Geol Soc London Spec Publ 179:155-174
23. Forster MA, Lister GS (2008) Tectonic sequence diagrams and the structural evolution of schists and gneisses in multiply deformed terranes. J Geol Soc London 165:923-939
24. Franěk J, Schulmann K, Lexa O, Tomek Č, Edel JB (2011) Model of syn-convergent extrusion of orogenic lower crust in the core of the Variscan belt: implications for exhumation of high-pressure rocks in large hot orogens. J Metamorph Geol 29:53-78
25. Franke W (2000) The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution. In: Franke W, Haak V, Oncken O, Tanner D (eds) Orogenic processes: quantification and modelling in the Variscan belt. Geol Soc London Spec Publ 179:35-61
26. Franke W, Zelazniewicz A (2002) Structure and evolution of the Bohemian arc. In: Winchester JA, Pharaoh TC, Verniers J (eds) Palaeozoic amalgamation of Central Europe. Geol Soc London Spec Publ 201: 279-293
27. Gebauer D (1993) Geochronologische Übersicht. In: Bauberger W (ed) Geologische Karte von Bayern 1:25000, Erläuterungen zum Blatt Nr. 6439 Tännesberg Bayer. Geol L Amt, München, pp 10-22
28. Glodny J, Grauert B, Fiala J, Vejnar Z, Krohe A (1998) Metapegmatites in the western Bohemian massif: ages of crystallisation and metamorphic overprint, as constrained by U-Pb zircon, monazite, garnet, columbite and Rb-Sr muscovite data. Geol Rundsch 87:124-134
29. Hajná J, Žák J, Kachlík V, Chadima M (2010) Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: the Teplá-Barrandian unit, Bohemian Massif. Precambrian Res 176:27-45
30. Hajná J, Žák J, Kachlík V (2011) Structure and stratigraphy of the Teplá-Barrandian Neoproterozoic: a new plate-tectonic reinterpretation. Gondwana Res 19:495-508
31. Havlíček V (1963) Tectogenetic disruption of the Barrandian Paleozoic. J Geol Sci 1:77-102
32. Havlíček V (1981) Development of a linear sedimentary depression exemplified by the Prague basin (Ordovician-Middle Devonian; Barrandian area-central Bohemia). J Geol Sci 35:7-48
33. Hofmann M, Linnemann U, Gerdes A, Ullrich B, Schauer M (2009) Timing of dextral strike-slip processes and basement exhumation in the Elbe Zone (Saxo-Thuringian Zone): the final pulse of the Variscan Orogeny in the Bohemian Massif constrained by LASF- ICP-MS U-Pb zircon data. Geol Soc London Spec Publ 327:197-214
34. Holubec J (1995) Structure (the Teplá-Barrandian Zone). In: Dallmeyer RD, Franke W, Weber K (eds) Pre-Permian geology of central and eastern Europe. Springer, Berlin, pp 392-397
35. Hrouda F (1982) Magnetic anisotropy of rocks and its application in geology and geophysics. Geophys Surv 5:37-82
36. Jackson M, Tauxe L (1991) Anisotropy of magnetic susceptibility and remanence: developments in the characterization of tectonic, sedimentary, and igneous fabric. Rev Geophys 29:371-376
37. Kachlík V (1996) Contact metamorphic host rocks of the Lestkov massif and their significance for reconstruction of tectonometamorphic evolution of the Teplá-Barrandian unit. Geoscience Research Reports for 1996, pp 81-82
38. Kachlík V (1999) Relationship between Moldanubicum, the Kutná Hora crystalline unit, and Bohemicum (Central Bohemia, Czech Republic): a result of the polyphase nappe tectonics. J Czech Geol Soc 44:201-289
39. Klomínský J (1963) Geology of the Čistá Massif. J Geol Sci 3:75-99
40. Klomínský J, Jarchovský T, Rajpoot GS (2010) The atlas of plutonic rocks and orthogneisses in the Bohemian Massif. Radioactive Waste Repository Authority of the Czech Republic, Technical Report No. TR-01-2010, Prague
41. Konopásek J, Schulmann K (2005) Contrasting Early Carboniferous field geotherms: evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (central European Variscides). J Geol Soc London 162:463-470
42. Kopecký L (1987) The Čistá ring structure, Czechoslovakia. In: Proceedings of the 1st Seminar on carbonatites and alkaline rocks of the Bohemian Massif and ambient regions. Czech Geological Survey, Prague, pp 23-58
43. Kopecký L, Dobeš M, Fiala J, Št'ovíčková N (1970) Fenites of the Bohemian Massif and the relations between fenitization, alkaline volcanism and deep fault tectonics. J Geol Sci 16:51-107
44. Kopecký L, Chlupáčová M, Klomínský J, Sokol A (1997) The Čistá-Jesenice pluton in western Bohemia: geochemistry, geology, petrophysics and ore potential. J Geol Sci 31:97-127
45. Košler J, Bowes DR, Farrow CM, Hopgood AM, Rieder M, Rogers G (1997) Constraints on the timing of events in the multi-episodic of the Teplá-Barrandian complex, western Bohemia, from integration of deformational sequence and Rb-Sr isotopic data. N Jb Miner Mh 5:203-220
46. Kretz R (1983) Symbols for rock forming minerals. Am Miner 68:277-279
47. Lüneburg CM, Lebit HDW (1998) The development of a single cleavage in an area of repeated folding. J Struct Geol 20:1531-1548
48. Martínez Catalán JR (2011) Are the oroclines of the Variscan belt related to late Variscan strike-slip tectonics? Terra Nova 23:241-247
49. Matte P (1986) Tectonic and plate tectonic model for the Variscan belt of Europe. Tectonophysics 126:329-374
50. Matte P, Maluski H, Rajlich P, Franke W (1990) Terrane boundaries in the Bohemian Massif: result of large-scale Variscan shearing. Tectonophysics 177:151-170
51. Miller RB, Paterson SR, Lebit H, Alsleben H, Lüneburg C (2006) Significance of composite lineations in the mid- to deep crust: a case study from the North Cascades, Washington. J Struct Geol 28:302-322
52. Murphy JB, Pisarevsky SA, Nance RD, Keppie JD (2004) Neoproterozoic-Early Paleozoic evolution of peri-Gondwanan terranes: implications for Laurentia-Gondwana connections. Int J Earth Sci 93:659-682
53. Nance RD, Murphy JB, Strachan RA, D'Lemos RS, Taylor GK (1991) Late Proterozoic tectonostratigraphic evolution of the Avalonian and Cadomian terranes. Precambrian Res 53:41-78
54. Nance RD, Gutiérrez-Alonso G, Keppie JD, Linnemann U, Murphy JB, Quesada C, Strachan A, Woodcock NH (2010) Evolution of the Rheic Ocean. Gondwana Res 17:194-222
55. Neubauer F (2002) Evolution of late Neoproterozoic to early Paleozoic tectonic elements in Central and Southeast European Alpine mountain belts: review and synthesis. Tectonophysics 352:87-103
56. Ordynec GJ, Žukova VI, Habásko J (1984) Prevariscan uranium mineralisation in the Proterozoic of the Bohemian Massif. J Miner Geol 29:69-77
57. Park RG (1969) Structural correlation in metamorphic belts. Tectonophysics 7:323-338
58. Passchier CW, Trouw RAJ (2005) Microtectonics. Springer, Berlin
59. Pertoldová J, Verner K, Vrána S, Buriánek D, Štědrá V, Vondrovic L (2010) Comparison of lithology and tectonometamorphic evolution of units at the northern margin of the Moldanubian Zone: implications for geodynamic evolution in the northeastern part of the Bohemian Massif. J Geosci 55:299-319
60. Pharaoh TC (1999) Palaeozoic terranes and their lithospheric boundaries within the Trans-European Suture Zone (TESZ): a review. Tectonophysics 177:263-292
61. Pin C, Waldhausrová J (2007) Sm-Nd isotope and trace element study of Late Proterozoic metabasalts ("spilites") from the Central Barrandian domain (Bohemian Massif, Czech Republic). In: Linnemann U, Nance D, Kraft P, Zulauf G (eds) The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to Alleghenian-Variscan collision. Geol Soc Am Spec Paper 423:231-247
62. Pin C, Kryza R, Oberc-Dziedzic T, Mazur S, Turniak K, Waldhausrová J (2007) The diversity and geodynamic significance of Late Cambrian (ca. 500 Ma) felsic anorogenic magmatism in the northern part of Bohemian Massif: a review based on Sm-Nd isotope and geochemical data. In: Linnemann U, Nance D, Kraft P, Zulauf G (eds) The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to Alleghenian-Variscan collision. Geol Soc Am Spec Paper 423:209-229
63. Pitra P, Burg JP, Schulmann K, Ledru P (1994) Late orogenic extension in the Bohemian Massif: petrostructural evidence in the Hlinsko region. Geodyn Acta 7:15-30
64. Pitra P, Burg JP, Giraud M (1999) Late-Variscan strike-slip tectonics between the Teplá-Barrandian and Moldanubian terranes (Czech Bohemian Massif): petrostructural evidence. J Geol Soc London 156:1003-1020
65. Potts GJ, Reddy SM (1999) Construction and systematic assessment of relative deformation histories. J Struct Geol 21:1245-1253
66. Powell CM (1979) A morphological classification of rock cleavage. Tectonophysics 58:21-34
67. Rajlich P (1987) Variscan ductile tectonics in the Bohemian Massif. Geol Rundsch 76:755-786
68. Rochette P, Jackson M, Aubourg C (1992) Rock magnetism and the interpretation of anisotropy of magnetic susceptibility. Rev Geophys 30:209-226
69. Scheuvens D, Zulauf G (2000) Exhumation, strain localization, and emplacement of granitoids along the western part of the Central Bohemian shear zone (Bohemian Massif). Int J Earth Sci 89:617-630
70. Schulmann K, Konopásek J, Janoušek V, Lexa O, Lardeaux JM, Edel JB, Štípská P, Ulrich S (2009) An Andean type Palaeozoic convergence in the Bohemian Massif. CR Geosci 341:266-286
71. Siebel W, Blaha U, Chen F, Rohrmüller J (2005) Geochronology and geochemistry of a dyke-host rock association and implications for the formation of the Bavarian Pfahl shear zone, Bohemian Massif. Int J Earth Sci 94:8-23
72. Stampfli GM, Kozur HW (2006) Europe from the Variscan to the Alpine cycles. Geol Soc London Mem 32:57-82
73. Strnad L, Mihajlevi ČM (2005) Sedimentary provenance of Mid-Devonian clastic sediments in the Teplá-Barrandian Unit (Bohemian Massif): U-Pb and Pb-Pb geochronology of detrital zircons by laser ablation ICP-MS. Mineral Petrol 84:47-68
74. Suchý V, Dobeš P, Filip J, Stejskal M, Zeman A (2002) Conditions for veining in the Barrandian Basin (Lower Paleozoic), Czech Republic: evidence from fluid inclusion and apatite fission track analysis. Tectonophysics 348:25-50
75. Tarling DH, Hrouda F (1993) The magnetic anisotropy of rocks. Chapman and Hall, London
76. Timmermann H, Štědrá V, Gerdes A, Noble SR, Parrish RR, Dörr W (2004) The problem of dating high-pressure metamorphism: a U-Pb isotope and geochemical study on eclogites and related rocks of the Mariánské Lázně Complex, Czech Republic. J Petrol 45:1311-1338
77. Timmermann H, Dörr W, Krenn E, Finger F, Zulauf G (2006) Conventional and in situ geochronology of the Teplá crystalline unit, Bohemian Massif: implications for the processes involving monazite formation. Int J Earth Sci 95:629-647
78. Tobisch OT, Paterson SR (1988) Analysis and interpretation of composite foliations in areas of progressive deformation. J Struct Geol 10:745-754
79. Venera Z, Schulmann K, Kröner A (2000) Intrusion within a transtensional tectonic domain: the Čistá granodiorite (Bohemian Massif)-structure and rheological modelling. J Struct Geol 22:1437-1454
80. Verner K, Žák J, Hrouda F, Holub FV (2006) Magma emplacement during exhumation of the lower- to mid-crustal orogenic root: the Jihlava syenitoid pluton, Moldanubian Unit, Bohemian Massif. J Struct Geol 28:1553-1567
81. Vernon RH (2004) A practical guide to rock microstructure. Cambridge University Press, Cambridge
82. Wenzel T, Mertz DF, Oberhänsli R, Becker T, Renne PR (1997) Age, geodynamic setting, and mantle enrichment processes of a K-rich intrusion from the Meissen massif (northern Bohemian massif) and implications for related occurrences from the mid- European Hercynian. Geol Rundsch 86:556-570
83. Williams PF (1985) Multiply deformed terrains-problems of correlation. J Struct Geol 7:269-280
84. Winchester JA, PACE TMR Network Team (2002) Paleozoic amalgamation of Central Europe: new results from recent geological and geophysical investigations. Tectonophysics 360:5-22
85. Winchester JA, Pharaoh TC, Verniers J, Ioane D, Seghedi A (2006) Palaeozoic accretion of Gondwana-derived terranes to the East European Craton: recognition of detached terrane fragments dispersed after collision with promontories. Geol Soc London Mem 32:323-332
86. Žák J, Schulmann K, Hrouda F (2005a) Multiple magmatic fabrics in the Sázava pluton (Bohemian Massif, Czech Republic): a result of superposition of wrench-dominated regional transpression on final emplacement. J Struct Geol 27:805-822
87. Žák J, Holub FV, Verner K (2005b) Tectonic evolution of a continental magmatic arc from transpression in the upper crust to exhumation of mid-crustal orogenic root recorded by episodically emplaced plutons: the Central Bohemian Plutonic Complex (Bohemian Massif). Int J Earth Sci 94:385-400
88. Žák J, Dragoun F, Verner K, Chlupáčová M, Holub FV, Kachlík V (2009) Forearc deformation and strain partitioning during growth of a continental magmatic arc: the northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif. Tectonophysics 469:93-111
89. Žák J, Kratinová Z, Trubač J, Janoušek V, Sláma J, Mrlina J (2011a) Structure, emplacement, and tectonic setting of Late Devonian granitoid plutons in the Teplá-Barrandian unit, Bohemian Massif. Int J Earth Sci 100: 1477-1495.
90. Žák J, Verner K, Finger F, Faryad SW, Chlupáčová M, Veselovský F (2011b) The generation of voluminous S-type granites in the Moldanubian unit, Bohemian Massif, by rapid isothermal exhumation of the metapelitic middle crust. Lithos 121: 25-40.
91. Žák J, Verner K, Holub FV, Kabele P, Chlupáčová M, Halodová P (2012) Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif. J Struct Geol 36: 27-42.
92. Zulauf G (1994) Ductile normal faulting along the West Bohemian Shear Zone (Moldanubian/Teplá-Barrandian boundary): evidence for late Variscan extensional collapse in the Variscan Internides. Geol Rundsch 83: 276-292.
93. Zulauf G (1997) From very low-grade to eclogite-facies metamorphism: tilted crustal sections as a consequence of Cadomian and Variscan orogeny in the Teplá-Barrandian unit (Bohemian Massif). Geotekt Forsch 89: 1-302.
94. Zulauf G (2001) Structural style, deformation mechanisms and paleostress along an exposed crustal section: constraints on the rheology of quartzofeldspathic rocks at supra- and infrastructural levels (Teplá-Barrandian unit, Bohemian Massif). Tectonophysics 332: 211-237.
95. Zulauf G, Dörr W, Fiala J, Vejnar Z (1997) Late Cadomian crustal tilting and Cambrian transtension in the Teplá-Barrandian unit (Bohemian Massif, Central European Variscides). Geol Rundsch 86: 571-587.
96. Zulauf G, Schitter F, Riegler G, Finger F, Fiala J, Vejnar Z (1999) Age constraints on the Cadomian evolution of the Teplá-Barrandian unit (Bohemian Massif) through electron microprobe dating of metamorphic monazite. Z Dtsch Geol Ges 150: 627-640.
97. Zulauf G, Dörr W, Fiala J, Kotková J, Maluski H, Valverde-Vaquero P (2002a) Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic). Terra Nova 14: 343-354.
98. Zulauf G, Bues C, Dörr W, Vejnar Z (2002b) 10 km minimum throw along the West Bohemian shear zone: evidence for dramatic crustal thickening and high topography in the Bohemian Massif (European Variscides). Int J Earth Sci 91: 850-864.