Variscan Deformation phases in the southwestern Bohemian Massif: new constraints from sheared granitoids;Variszische dsen in der südwestlichen Böhmischen Masse: Neue randbedingungen aus zerscherten Granitoiden

Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften

Volumn 161, Issue 1, 2010, Pages 1-23

  Galadí Enríquez, Elena ^a   Dörr, Wolfgang ^b   Zulauf, Gernold ^b   Galindo Zaldívar, Jesús ^c   Heidelbach, Florian ^d   Rohrmüller, Johann ^a  

^a Bayerisches Landesamt für Umwelt ^*  (Germany)

^b GOETHE UNIVERSITY   (Germany)

^c UNIVERSITY OF GRANADA   (Spain)

^d UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Bohemian Massif; Deformation; Moldanubian Zone; Shear zone; U Pb monazite dating; Variscides

Indexed keywords

EID: 79251602022     PISSN: 18601804     EISSN: None     Source Type: Journal    
DOI: 10.1127/1860-1804/2010/0161-0001     Document Type: Article

References (82)

1. Beer, W.W. (1981): Die strukturelle Entwicklung der Metamorphite des Bayerischen Waldes: 186 p., Ph.D. thesis, Univ. Göttingen, Göttingen.
2. Behrmann, J.H. (1985): Crystal plasticity and superplasticity in quartzite: a natural example. Tectonophysics, 115: 101-129. Amsterdam (Elsevier).
3. Behrmann, J.H. & Mainprice, D. (1987): Deformation mechanisms in a high-temperature quartz-feldspar mylonite: evidence for superplastic flow in the lower continental crust. Tectonophysics, 140: 297-305. Amsterdam (Elsevier).
4. Berthé, D., Choukroune, P. & Jegouzo, P. (1979): Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone. J. Struct. Geol., 1: 31-42. Oxford (Pergamon).
5. Blaha, U. & Siebel, W. (2006): Geologische Karte von Bayern 1: 25 000, Blatt Nr. 7145 Schöfweg. Bayerisches L.-Amt Umwelt, München.
6. Bohlen, S.R., Montana, A. & Kerrick, D.M. (1991): Precise determinations of the equilibria kyanite-sillimanite and kyanite-andalusite and a revised triple point for Al2SiO5 polymorphs. American Mineral., 76: 677-680. Washington D. C. (Mineral. Soc. America).
7. Bouchez, J.L. & Pêcher, A. (1981): The Himalayan Main Central Thrust pile and its quartz-rich tectonites in central Nepal. Tectonophysics, 78: 23-50. Amsterdam (Elsevier).
8. Boullier, A.M. & Gueguen, Y. (1975): SP-Mylonites: origin of some mylonites by superplastic flow. Contrib. Mineral. Petrol., 50: 93-104. Berlin (Springer).
9. Brandmayr, M., Dallmeyer, R.D., Handler, R. & Wallbrecher, E. (1990): Age and kinematics of shear zones in the southern Bohemian Massif: evidence from the Rodl shear zone. Terranes in the circum-atlantic Paleozoic orogens, Int. Conf. on Paleozoic orogens in Central Europe, conf. abstr., Göttingen-Giessen Aug. Sept. 1990.
10. Brandmayr, M., Dallmeyer, R.D., Handler, R. & Wallbrecher, E. (1995): Conjugate shear zones in the Southern Bohemian Massif (Austria): implications for Variscan and Alpine tectonothermal activity. Tectonophysics, 248: 97-116. Amsterdam (Elsevier).
11. Brandmayr, M., Loizenbauer, J. & Wallbrecher, E. (1999): Contrasting P-T conditions during conjugate shear zone development in the Southern Bohemian Massif, Austria. Mitt. Österreichische geol. Ges., 90: 11-29. Wien (Österreichische Geol. Ges.).
12. Büttner, S.H. (1999): The geometric evolution of structures in granite during continuous deformation from magmatic to solid-state conditions: an example from the central European Variscan Belt. American Mineral., 84:1781-1792. Washington D. C. (Mineral. Soc. America).
13. Bundesanstalt für Geowissenschaften und Rohstoffe (1993): Geologische Karte der Bundesrepublik Deutschland 1: 1 000 000, Hannover.
14. Chatterjee, N.D. & Flux, S. (1986): Thermodynamic mixing properties of muscovite-paragonite crystalline solutions at high temperatures and pressures, and their geological applications. J. Petrol., 27: 677-693. Oxford (Oxford Univ. Press).
15. Chen, F. & Siebel, W. (2004): Zircon and titanite geochronology of the Fürstenstein granite massif, Bavarian Forest, SW Bohemian Massif: pulses of the late Variscan magmatic activity. Europ. J. Mineral., 16: 777-788. Stuttgart (Schweizerbart).
16. Chen, F., Siebel, W. & Satir, M. (2002): Zircon geochronology and geochemistry of the Fürstensteiner pluton, Bavarian Forest. Ber. dt. mineral. Ges., 14: 33. Stuttgart (Schweizerbart).
17. Christinas, P., Köhler, H. & Müller-Sohnius, D. (1991a): Alterstellung und Genese der Palite des Vorderen Bayerischen Waldes (Nordostbayern). Geol. Bavarica, 96: 87-107. München (Bayerisches Geol. L.-Amt).
18. Christinas, P., Köhler, H. & Müller-Sohnius, D. (1991b): Rb-Sr- Alterbestimmungen an Intrusiva des Hauzenberges Massivs, Nordostbayern. Geol. Bavarica, 96: 109-118. München (Bayerisches Geol. L.-Amt).
19. Dietl, C., Gößmann, M. & de Wall, H. (2005): Kombinierte active und passive Plutonplatznahme in einer verdickten Kruste - Erste Ergebnisse von gesteinsmagnetischen und petrologischen Untersuchungen am Fürstensteiner Intrusivkomplex (Bayerischer Wald). Z. dt. geol. Ges., 155 (2-4): 311-328. Stuttgart (Schweizerbart).
20. Dollinger, U. (1967): Das Hauzenberger Granitmassiv und seine Umrahmung. Geol. Bavarica, 58: 145-168. München (Bayerisches Geol. L.-Amt).
21. Finger, F., Roberts, M.P., Haunschmid, B., Schermaier, A. & Steyrer, H.P. (1997): Variscan granitoids of central Europe: their typology, potential sources and tectonothermal relations. Mineral. Petrol., 61: 67-96. Wien (Springer).
22. Finger, F., Gerdes, A., Janoušek, V., René, M. & Riegler, G. (2007): Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo-Moldanubian tectonometamorphic phases. J. Geosci., 52: 9-28. Prague (Czech Geol. Soc.).
23. Franke, W. (1992): Phanerozoic structures and events in central Europe. In: Blundell, D., Freeman, R. & Mueller, S. (eds.): A continent revealed - the European geotraverse: 164-179. Cambridge (Cambridge Univ. Pr.).
24. Frentzel, A. (1911): Das Passauer Granitmassiv. Geognost. Jh., 24: 105-192. München (Piloty & Loehle).
25. Freudenberger, W. & Schwerd, K. (1996): Erläuterungen zur Geologischen Karte von Bayern 1: 500 000, 4th ed.: 329 p. München (Bayerisches Geol. L.-Amt).
26. Friedl, G., von Quadt, A., Ochsner, A. & Finger, F. (1993): Timing of the Variscan orogeny in the Southern Bohemian Massif (NEAustria) deduced from new U-Pb zircon and monazite dating. Terra Abstr., Abstr. Suppl. No. 1, Terra Nova, 5: 235-236. Oxford (Blackwell).
27. Galadí-Enríquez, E. (2007): Granitoids from the European Variscides: an approach to their emplacement and tectonometamorphic history: 240 p., on-line published Ph.D. thesis, Univ. Frankfurt am Main.
28. Galadí-Enríquez, E. & Zulauf, G. (2006): Geologische Karte von Bayern 1: 25 000, Blatt Nr. 7246 Tittling. Bayerisches L.- Amt Umwelt, München.
29. Galadí-Enríquez, E., Zulauf, G., Heidelbach, F. & Rohrmüller, J. (2006): Insights into the post-emplacement history of the Saunstein granitic dyke showing heterogeneous deformation and inconsistent shear-sense indicators (Bavarian Forest, Germany). J. Struct. Geol., 28: 1536-1552. Oxford (Pergamon).
30. Galadí-Enríquez, E., Blaha, U., Siebel, W. & Rohrmüller, J. (2009): Structural, geochronological and barometric constraints on Variscan deformation in the southwestern Bohemian Massif: the case study of the Untermitterdorf igneous body (Bavarian Forest, Germany). Z. dt. Ges. Geowiss., 160 (4): 297-313. Stuttgart (Schweizerbart).
31. Grauert, B., Hänny, R. & Soptrajanova, G. (1974): Geochronology of a polymetamorphic and anatectic gneiss region: the Moldanubicum of the area Lam-Deggendorf, Eastern Bavaria, Germany. Contrib. Mineral. Petrol., 45: 37-63. Berlin (Springer).
32. Handler, R., Brandmayr, M. & Wallbrecher, E. (1991): The Rodl shear zone in the southern Bohemian Massif. Zbl. Geol. Paläont., Teil 1 (1): 69-86. Stuttgart (Schweizerbart).
33. Harre, W., Kreuzer, H., Lenz, H. & Müller, P. (1967): Zwischenbericht über K/Ar und Rb/Sr-Datierungen von Gesteinen aus dem ostbayerisch-österreichischen Kristallin. B.-Anst. Bodenforsch., Datierungsber. 5/67: Archiv-Nr. 25/338, Hannover (B.-Anst. Bodenforsch.).
34. Hemingway, B.S., Robie, R.A., Evans, H.T. & Kerrick, D.M. (1991): Heat capacities and entropies of sillimanite, fibrolite, andalusite, kyanite, and quartz and the Al2SiO5 phase diagram. American Mineral., 76: 1597-1613. Washington D. C. (Mineral. Soc. America).
35. Hoffmann, R. (1962): Die Tektonik des Bayerischen Pfahls. Geol. Rdsch., 52: 332-346. Stuttgart (Enke).
36. Horn, P., Köhler, H. & Müller-Sohnius, D. (1986): Rb/Sr-Isotopengeochemie hydrothermaler Quarze des bayerischen Pfahles und eines Flusspat-Schwerspat-Ganges von Nabburg-Wölsendorf /Bundesrepublik Deutschland. Chem. Geol. (Isotope Geosci. Sect.), 58: 259-272. Amsterdam (Elsevier).
37. Janoušek, V., Gerdes, A., Vrána, S., Finger, F., Erban, V., Friedl, G. & Braithwaite, C.J.R. (2006): Low-pressure granulites of the Lišov Massif, Southern Bohemia: Viséan metamorphism of Late Devonian Plutonic arc rocks. J. Petrol., 47: 705-744. Oxford (Oxford Univ. Press).
38. Jessell, M.W. & Lister, G.S. (1990): A simulation of the temperature dependence of quartz fabrics. In: Knipe, R.J. & Rutter, E.H. (eds.): Deformation mechanisms, rheology and tectonics. Geol. Soc. London, Spec. Publ., 54: 353-362. London (Geol. Soc. London).
39. Johannes, W. & Holtz, F. (1996): Petrogenesis and experimental petrology of granitic rocks. Minerals and rocks, 22: 335 p. Berlin (Springer).
40. Kalt, A., Corfu, F. & Wijbrans, J.R. (2000): Time calibration of a P-T path from a Variscan high-temperature low-pressure metamorphic complex (Bayerische Wald, Germany), and the detection of inherited monazite. Contrib. Mineral. Petrol., 138: 143-163. Berlin (Springer).
41. Klein, T., Kiehm, S., Siebel, W., Shang, C.K., Rohrmüller, J., Dörr, W. & Zulauf, G. (2008): Age and emplacement of late-Variscan granites of the western Bohemian Massif with main focus on the Hauzenberg granitoids (European Variscides, Germany). Lithos, 102: 478-507. Amsterdam (Elsevier).
42. Kretz, R. (1983): Symbols for rock-forming minerals. American Mineral., 68: 277-279. Washington D. C. (Mineral. Soc. America).
43. Law, R.D. (1990): Crystallographic fabrics: a selective review of their applications to research in structural geology. In: Knipe, R.J. & Rutter, E.H. (eds.): Deformation mechanisms, rheology and tectonics. Geol. Soc. London, Spec. Publ., 54: 335-352. London (Geol. Soc. London).
44. Le Maitre, R.W., Streckeisen, A., Zanettin, B., Le Bas, M.J., Bonin, B., Bateman, P., Bellieni, G., Dudek, A., Efremova, S., Keller, J., Lameyre, J., Sabine, P.A., Schmid, R., Sørensen, H. & Woolley, A.R. (2002): Igneous Rocks. A classification and glossary of terms: 236 p., Cambridge (Cambridge Univ. Pr.).
45. Lister, G.S. & Snoke, A.W. (1984): S-C mylonites. J. Struct. Geol., 6: 617-638. Oxford (Pergamon).
46. Ludwig, K.R. (1980): Calculation of uncertainties of U-Pb isotope data. Earth Planetary Sci. Lett., 46: 212-220. Amsterdam (Elsevier).
47. Ludwig, K.R. (2001): User's manual for Isoplot/Ex version 2.49, a geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center, Spec. Publ., 1a: 55 p. Berkley (CA) (BGC).
48. Masch, L. & Cetin, B. (1991): Gefüge, Deformationsmechanismen und Kinematik in ausgewählten Hochtemperatur-Mylonitzonen im Moldanubikum des Bayerischen Waldes. Geol. Bavarica, 96: 7-27. München (Bayerisches Geol. L.-Amt).
49. Massonne, H.J. (1984): Bestimmung von Intrusionstiefen variszischer Granite Mitteleuropas und Neuschottlands anhand der Chemie ihrer Hellglimmer. Fortschr. Mineral., Beih., 62 (1): 147-149. Stuttgart (Schweizerbart).
50. Massonne, H.J. & Schreyer, W. (1979): Synthese von Phengiten im System K2O-MgO-Al2O3-SiO2-H2O bei Wasserdrucken bis 35 kbar. Fortschr. Mineral., Beih., 57 (1): 98-99. Stuttgart (Schweizerbart).
51. Massonne, H.J. & Schreyer, W. (1987): Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite and quartz. Contrib. Mineral. Petrol., 96: 212-224. Berlin (Springer).
52. Massonne, H.J. & Szpurka, Z. (1997): Thermodynamic properties of white micas on the basis of high-pressure experiments in the systems K2O-MgO-Al2O3-SiO2-H2O and K2O-FeO-Al2O3-SiO2-H2O. Lithos, 41: 229-250. Amsterdam (Elsevier).
53. Matte, P. (2001): The Variscan collage and orogeny (480-290 Ma) and the tectonic definition of the Armorica microplate: a review. Terra Nova, 13: 122-128. Oxford (Blackwell).
54. Mattern, F. (1995): Late Carboniferous to early Triassic shear sense reversals at strike-slip faults in eastern Bavaria. Zbl. Geol. Paläont., Teil 1, 1993: 1471-1490. Stuttgart (Schweizerbart).
55. Passchier, C.W. & Trouw, R.A.J. (1996): Microtectonics: 289 p. Berlin (Springer).
56. Platt, J.P. (1984): Secondary cleavages in ductile shear zones. J. Struct. Geol., 6: 439-442. Oxford (Pergamon).
57. Prior, D.J., Boyle, A.P., Brenker, F., Cheadle, M.C., Day, A., López, G., Peruzzo, L., Potts, G.J., Reddy, S., Spiess, R., Timms, N.E., Trimby, P., Wheeler, J. & Zetterström, L. (1999): The application of electron backscatter diffraction and orientation contrast imaging in the SEM to textural problems in rocks. American Mineral., 84: 1741-1759. Washington D. C. (Mineral. Soc. America).
58. Propach, G. (2002): Postmagmatic mineral parageneses of dykes may be used to estimate the PT data of their country rocks - an example from the Bayerischer Wald, Germany. N. Jb. Mineral. Abh., 9: 424-432. Stuttgart (Schweizerbart).
59. Propach, G., Baumann, A., Schulz-Schmalschläger, M. & Grauert, B. (2000): Zircon and monazite U-Pb ages of Variscan granitoid rocks and gneisses in the Moldanubian zone of eastern Bavaria, Germany. N. Jb. Geol. Paläont. Mh., 6: 345-377. Stuttgart (Schweizerbart).
60. Propach, G., Bayer, B., Chen, F., Frank, C., Hölzl, S., Hofmann, B., Köhler, H., Siebel, W. & Troll, G. (2008): Geochemistry and petrology of late Variscan magmatic dykes of the Bavarian Forest, Germany. Geol. Bavarica, 110: 304-342. Augsburg (Bayerisches L.-Amt Umwelt).
61. Schmid, S.W. & Casey, M. (1986): Complete fabric analysis of some commonly observed quartz c-axis patterns. Geophys. Monogr., 36: 263-286. Washington D. C. (American Geophys. Union).
62. Siebel, W. (1998): Variszischer spät- bis postkollisionaler Plutonismus in Deutschland: Regionale Verbreitung, Stoffbestand und Altersstellung. Z. geol. Wiss., 26: 329-358. Berlin.
63. 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. Berlin (Springer).
64. Simpson, C. & Schmid, S.M. (1983): An evaluation of criteria to deduce the sense of movement in sheared rocks. Geol. Soc. America Bull., 94: 1281-1288. Boulder (CO) (Geol. Soc. America).
65. Simpson, G.D.H., Thompson, A.B. & Connolly, J.A.D. (2000): Phase relations, singularities and thermobarometry of metamorphic assemblages containing phengite, chlorite, biotite, Kfeldspar, quartz and H2O. Contrib. Mineral. Petrol., 139: 555-569. Berlin (Springer).
66. Stacey, J.S. & Kramers, J.D. (1975): Approximation of terrestrial lead isotope evolution by a two stage model. Earth Planetary Sci. Lett., 127: 30-45. Amsterdam (Elsevier).
67. Steiger, R.H. & Jäger, E. (1997): Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planetary Sci. Lett., 36: 359-362. Amsterdam (Elsevier).
68. Stein, E. (1988): Die strukturgeologische Entwicklung im Übergangsbereich Saxothuringikum / Moldanubikum in NE-Bayern. Geol. Bavarica, 92: 5-131. München (Bayerisches Geol. L.- Amt).
69. Stipp, M., Stünitz, H., Heilbronner, R. & Schmid, S.M. (2002): The eastern Tonale fault zone: a "natural laboratory" for crystal plastic deformation of quartz over a temperature range from 250 to 700°C. J. Struct. Geol., 24: 1861-1884. Oxford (Pergamon).
70. Suess, F.E. (1903): Bau und Bild der Böhmischen Masse. In: Diener, C., Hoernes, R., Suess, F.E. & Uhlig, V. (eds.): Bau und Bild Österreichs: 1-322. Wien (Temsky-Freytag).
71. Teipel, U., Eichhorn, R., Loth, G., Rohrmüller, J., Höll, R. & Kennedy, A. (2004): U-Pb SHRIMP and Nd isotopic data from the western Bohemian Massif (Bayerischer Wald, Germany): Implications for Upper Vendian and Lower Ordovician magmatism. Int. J. Earth Sci., 93: 782-801. Berlin (Springer).
72. Teipel, U., Galadí-Enríquez, E., Glaser, S., Kroemer, E. & Rohrmüller, J. (2008): Erdgeschichte des Bayerischen Waldes. Geologischer Bau, Gesteine, Sehenswürdigkeiten. Bayerisches L.-Amt Umwelt, Augsburg.
73. Troll, G. (1964): Das Intrusivgebiet von Fürstenstein (Bayerischer Wald). Geol. Bavarica, 52: 1-140. München (Bayerisches Geol. L.-Amt).
74. Tullis, J. (1983): Deformation of feldspars. In: Ribbe, P.H. (ed.): Feldspar mineralogy. Rev. Mineral., 2: 297-323. Washington D. C. (Mineral. Soc. America).
75. Vollbrecht, A., Weber, K. & Schmoll, J. (1989): Structural model for the Saxothuringian-Moldanubian suture in the Variscan basement of the Oberpfalz (Northeastern Bavaria, F.R.G.) interpreted from geophysical data. Tectonophysics, 157: 123-133. Amsterdam (Elsevier).
76. Wallbrecher, E., Brandmayr, M. & Handler, R. (1990): Kinematische Untersuchungen an Blattverschiebungszonen in der südlichen Böhmischen Masse. Österreichische Beitr. Meteorol. Geophys., 3: 97-120. Wien (Zentralanst. Meteorol. Geodyn.).
77. Zen, E. (1988): Phase relations of peraluminous granitic rocks and their petrogenetic implications. Annu. Rev. Earth Planetary Sci., 16: 21-51. Palo Alto (CA) (Annu. Rev. Inc.).
78. Ziegler, P.A. (1986): Geodynamic model for the Paleozoic crustal consolidation of Western and Central Europe. Tectonophysics, 126: 303-328. Amsterdam (Elsevier).
79. Ziegler, P.A. (1988): Post-Hercynian plate reorganization in the Tethys and Arctic-North Atlantic domains. In: Manspeizer, W.J.S. (ed.): Triassic-Jurassic rifting. Continental breakup and the origin of the Atlantic Ocean and passive margins: 711-755. Amsterdam (Elsevier).
80. Zulauf, G. (1992): Late- to post-Variscan deformation phases and paleostresses in the KTB pilot well (Bohemian Massif, Germany). Tectonophysics, 202: 1-21. Amsterdam (Elsevier).
81. Zulauf, G. (1993): Brittle deformation events at the western border of the Bohemian Massif Germany). Geol. Rdsch., 83: 489-504. Berlin (Springer).
82. Zulauf, G. (1997): Von der Anchizone bis zur Eklogitfazies: Angekippte Krustenprofile als Folge der cadomischen und variszischen Orogenese im Teplá-Barrandium (Böhmische Masse). Geotekt. Forsch., 89: 1-302. Stuttgart (Schweizerbart).