Saxothuringian provenance of suspected terranes in the Central Sudetes, Bohemian Massif: zircon evidence of a recycled subducted slab

• Autorzy: Mazur S. , Szczepański J. , Tumiak K. , McNaughton N. J.
• Języki publikacji: EN

Słowa kluczowe

EN

subducted; zircon; Central Sudetes

• Wydawca: Instytut Nauk Geologicznych PAN ; Instytut Nauk Geologicznych Uniwersytetu Wrocławskiego
• Czasopismo: Geologia Sudetica
• Rocznik: 2014
• Tom: Vol. 42
• Strony: 56--58
• Opis fizyczny: Bibliogr. 10 poz., rys.

Twórcy

autor

Mazur S.

• Institute of Geological Sciences, University of Wroclaw, 50-204 Wroclaw, Pl. Borna 9, Poland
• GETECH, Kitson House, Elmete Hall, Elmete Lane, Leeds LS8 2HJ, UK

autor

Szczepański J.

• Institute of Geological Sciences, University of Wroclaw, 50-204 Wroclaw, Pl. Borna 9, Poland

autor

Tumiak K.

• Institute of Geological Sciences, University of Wroclaw, 50-204 Wroclaw, Pl. Borna 9, Poland

autor

McNaughton N. J.

• John de Laeter Centre for Mass Spectrometry, Curtin University, GPO Box U1987 Perth, Western Australia 6845

Bibliografia

• 1. BUSCHMANN, B., NASDALA, L., JONAS, P., LINNEMANN, U. & GEHMLICH, M., 2001. SHRIMP U-Pb dating of tuff- derived and detrital zircons from Cadomian marginal basin fragments (Neoproterozoic) in the northeastern Saxothurin Monatshefte: 321-342.
• 2. DON, J., SKÁCEL, J. & GOTOWAŁA, R., 2003. The boundary zone of the East and West Sudetes on the 1:50 000 scale geolog ical map of the Velké Vrbno, Staré Mesto and Snieżnik Metamorphic Units. Geologia Sudetica, 35: 25-59.
• 3. ELICKI, O., 1997. Biostratigraphic data of the German Cambrian present state of knowledge. Freiberger Forschungshefte, 466: 155-165.
• 4. KRYZA, R., MAZUR, S. & PIN, C., 2003. Subduction- and non- subduction-related igneous rocks in the Central-European Variscides: geochemical and Nd isotope evidence for a composite origin of the Kłodzko Metamorphic Complex, Polish Sudetes. Geodinamica Acta, 16: 39-57.
• 5. LINNEMANN, U. & ROMER, R. L., 2002. The Cadomian orogeny in Saxo-Thuringia, Germany: Geochemical and Nd-Sr-Pb isotopic characterization of marginal basins with constraints to geotectonic setting and provenance. Tectonophysics, 352: 33-64.
• 6. LINNEMANN, U., GERDES, A., DROST, K.& BUSCHMANN, B., 2007. Cadomian orogenic processes - The ult imate cause for the opening of the Rheic Ocean: Constraints by Laser Abla- tion-ICP-MS U-Pb zircon dating and analysis of the geo- tectonic setting (Saxo-Thuringian zone, Bohemian massif, Germany). In: Linnemann, U., Kraft, P., Nance, R.D., Zulauf, G., (Eds.), The Geology of Peri-Gondwana: The Avalonian- Cadomian Belt, Adjoining Cratons and the Rheic Ocean, Geological Society of America, Special Papers, 423: 61-96.
• 7. MAZUR, S., SZCZEPAŃSKI, J., TURNIAK, K. & MCNAUGH- TON, N. J., 2012. Location of the Rheic suture in the eastern Bohemian Massif: evidence from detrital zircon data. Terra Nova, 24: 199-206.
• 8. MAZUR, S., TURNIAK, K., SZCZEPAŃSKI, J. & MCNAUGH- TON, N. J., 2013. Vestiges of Saxothuringian crust in the Central Sudetes, Bohemian Massif: Zircon evidence of a recycled subducted slab provenance. Gondwana Research, in press: http ://dx.doi.org/10. 1016/j .gr.2013. 11.005.
• 9. MURTEZI, M., 2006. The acid metavolcanic rocks of the Orlica- Snieżnik Dome: their origin and tectonometamorphic evolu tion. Geologia Sudetica, 38: 1-38.
• 10. SZCZEPAŃSKI, J., 2010. Provenance and tectonometamorphic evolution of the supracrustal series from the Bystrzyckie Mts. Crystalline Massif. Wrocławska Drukarnia Naukowa PAN, Wrocław, 166 pp